Symposium program

The symposium contains different kinds of presentations, social activities and side meetings, as shown in the figure below.
- green: key note presentations and poster presentations
- blue: oral presentations in parallel sessions
- organge: social activites
- yellow: side meetings (not part of the official symposium program)

Full session program with all deatails and abstracts

Week at a glance

Presentations (Status 30 May)

  • All abstracts (list sorted by ID)

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    td height=28 width=52 class=xl65 style=height:21.0pt; width:39ptDay/td

    td width=61 class=xl67 style=width:46ptTime/td

    td width=177 class=xl65 style=width:133ptPresenter/td

    td width=593 class=xl66 style=width:445ptTitle/td

    td width=65 class=xl65 style=width:49ptID/td

    /tr

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    td height=37 width=52 class=xl72 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptWillmes et al./td

    td width=593 class=xl70 style=width:445ptShaping the sea ice: How ocean

    and atmosphere drive the patterns of wintertime Arctic sea ice leads./td

    td width=65 class=xl70 style=width:49pt92a4001/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptWyburn-Powell et al./td

    td width=593 class=xl70 style=width:445ptLarge Scale Climate Modes as

    Drivers of Low-Frequency Regional Arctic Sea Ice Variability/td

    td width=65 class=xl70 style=width:49pt92a4002/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptArndt et al./td

    td width=593 class=xl70 style=width:445ptLearning from local SNOW

    properties For Large-scale Antarctic ice pacK volumE: The SNOWflAke project/td

    td width=65 class=xl70 style=width:49pt92a4006/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt10:00/td

    td width=177 class=xl72 style=width:133ptArndt et al./td

    td width=593 class=xl70 style=width:445ptRelevance of inherent snow

    property variability for the large-scale Antarctic sea ice mass budget/td

    td width=65 class=xl70 style=width:49pt92a4007/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptArndt et al./td

    td width=593 class=xl70 style=width:445ptSnow depth vs. snow accumulation

    in the Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4008/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptArndt et al./td

    td width=593 class=xl70 style=width:445ptSeasonal and interannual

    variability of landfast sea ice properties in Atka Bay and its relation to

    the adjacent ice shelf and ocean beneath/td

    td width=65 class=xl70 style=width:49pt92a4009/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptZahabi et al./td

    td width=593 class=xl70 style=width:445ptCombatting Kessler Syndrome

    amp; the Implementation of Spaceport Infrastructure in the High North/td

    td width=65 class=xl70 style=width:49pt92a4015/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt9:40/td

    td width=177 class=xl72 style=width:133ptCampbell et al./td

    td width=593 class=xl70 style=width:445ptBiogeochemical regimes of sea

    ice microhabitats in the High Arctic/td

    td width=65 class=xl70 style=width:49pt92a4017/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptWiehle et al./td

    td width=593 class=xl70 style=width:445ptTowards Sea Ice Classification

    using combined Sentinel-1 and Sentinel-3 data/td

    td width=65 class=xl70 style=width:49pt92a4018/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptHowell et al./td

    td width=593 class=xl70 style=width:445ptA comparison of Arctic Ocean sea

    ice outflow between Nares Strait andspannbsp;

    /spanthe Canadian Arctic Archipelago/td

    td width=65 class=xl70 style=width:49pt92a4019/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMaaß et al./td

    td width=593 class=xl70 style=width:445ptComparison of snow height buoy

    measurements with 1D snow cover simulations in the Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4020/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptMaus et al./td

    td width=593 class=xl70 style=width:445ptMicrostructure-based

    parametrisation of the salinity of young growing sea ice/td

    td width=65 class=xl70 style=width:49pt92a4022/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:00/td

    td width=177 class=xl72 style=width:133ptAllard et al./td

    td width=593 class=xl70 style=width:445ptDevelopment and testing of

    spatially varying landfast ice parameters in CICE6/td

    td width=65 class=xl70 style=width:49pt92a4023/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptde Rijke-Thomas et al./td

    td width=593 class=xl70 style=width:445ptAirborne investigation of

    quasi-specular Ku-band radar scattering for satellite altimetry over

    snow-covered Arctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4025/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptRiihelä et al./td

    td width=593 class=xl70 style=width:445ptVariability and trends in Arctic

    and Antarctic sea ice albedo, 1979-2020, from the third edition of the CLARA

    data record/td

    td width=65 class=xl70 style=width:49pt92a4026/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptAllard et al./td

    td width=593 class=xl70 style=width:445ptCalibrating the biogeochemical

    indicators of seasonal sea ice cover in the sedimentary archives of a

    subarctic harbour, Bay of Sept-Îles, Quebec (Canada)/td

    td width=65 class=xl70 style=width:49pt92a4027/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLohse et al./td

    td width=593 class=xl70 style=width:445ptAutomated ice type mapping for

    navigational support of vessels in the Arctic: Application and validation

    during the CIRFA-22 cruise/td

    td width=65 class=xl70 style=width:49pt92a4029/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptToyota et al./td

    td width=593 class=xl70 style=width:445ptA study on the properties of

    granular ice from laboratory experiments/td

    td width=65 class=xl70 style=width:49pt92a4030/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptXu et al./td

    td width=593 class=xl70 style=width:445ptSimulating Arctic Sea Ice

    Kinematics at Kilometer Resolution in CESM2-CICE5 – Sensitivity to Rheology

    and Strength Parameterization/td

    td width=65 class=xl70 style=width:49pt92a4031/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptXu et al./td

    td width=593 class=xl70 style=width:445ptA Climate Record of

    Wave-Affected Marginal Ice Zone in the Atlantic Arctic based on CryoSat-2/td

    td width=65 class=xl70 style=width:49pt92a4032/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptBrady et al./td

    td width=593 class=xl70 style=width:445ptPan-Arctic sea ice motion from

    synthetic aperture radar using the Environment and Climate Change Canada

    automated sea ice tracking system/td

    td width=65 class=xl70 style=width:49pt92a4033/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptBischof et al./td

    td width=593 class=xl70 style=width:445ptSeasonal variations in the sea

    ice-mixed layer depth relationship in the West Antarctic Peninsula/td

    td width=65 class=xl70 style=width:49pt92a4034/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBelter et al./td

    td width=593 class=xl70 style=width:445ptFastCast-2: Optimized route

    suggestions for ships in polar regions using AI- based processing, Earth

    Observation data, and model forecasts/td

    td width=65 class=xl70 style=width:49pt92a4036/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptEis et al./td

    td width=593 class=xl70 style=width:445ptOptimized routes for ship in-ice

    navigation based on sea ice classification and ice drift forecasts/td

    td width=65 class=xl70 style=width:49pt92a4037/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptCheng et al./td

    td width=593 class=xl70 style=width:445ptTemperature and salinity in the

    Bohai Sea, the lowest latitude ice-covered sea in the Pan-Eurasian EXperiment

    (PEEX) domain: observation and modelling/td

    td width=65 class=xl70 style=width:49pt92a4038/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptHolmes et al./td

    td width=593 class=xl70 style=width:445ptReducing uncertainty in

    projections of Antarctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4039/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptMchedlishvili et al./td

    td width=593 class=xl70 style=width:445ptResolving drag coefficients

    estimates on Arctic-wide spatial and Monthly temporal scales/td

    td width=65 class=xl70 style=width:49pt92a4040/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptKortum et al./td

    td width=593 class=xl70 style=width:445ptRealising the Potential of Data

    Driven Sea Ice Retrieval Methods from SAR/td

    td width=65 class=xl70 style=width:49pt92a4041/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptNab et al./td

    td width=593 class=xl70 style=width:445ptAssimilation of CryoSat-2,

    Sentinel-3, ICESat-2 and SMOS sea ice thickness into an ice-ocean forecast

    model/td

    td width=65 class=xl70 style=width:49pt92a4042/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBabb et al./td

    td width=593 class=xl70 style=width:445ptUsing a New Year-Round Sea Ice

    Thickness Product to Quantify the Complete Annual Record of Sea Ice Volume

    Export Through Fram Strait (2010-2021)/td

    td width=65 class=xl70 style=width:49pt92a4043/td

    /tr

    tr height=19 style=page-break-before:always; height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptvon Albedyll et al./td

    td width=593 class=xl70 style=width:445ptNew ice production in leads

    estimated from SAR-derived sea ice divergence/td

    td width=65 class=xl70 style=width:49pt92a4045/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRostosky et al./td

    td width=593 class=xl70 style=width:445ptInfluence of warm air intrusions

    on satellite sea ice concentration climatologies/td

    td width=65 class=xl70 style=width:49pt92a4046/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptPerron et al./td

    td width=593 class=xl70 style=width:445ptInverting spectral albedo to

    estimate solar heat deposition at the surface of sea ice/td

    td width=65 class=xl70 style=width:49pt92a4047/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLiu et al./td

    td width=593 class=xl70 style=width:445ptAtmospheric turbulent

    intermittency over the Arctic sea-ice surfacespannbsp;

    /spanduring the MOSAiC expedition/td

    td width=65 class=xl70 style=width:49pt92a4049/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:45/td

    td width=177 class=xl72 style=width:133ptMeiners et al./td

    td width=593 class=xl70 style=width:445ptImplications of Antarctic

    sea-ice change on Southern Ocean ecology and biogeochemical cycles/td

    td width=65 class=xl70 style=width:49pt92a4050/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptLosch et al./td

    td width=593 class=xl70 style=width:445ptHeterogeneity and linear

    kinematic features in sea ice models with Viscous-Plastic and

    Maxwell-Elasto-Brittle rheologies/td

    td width=65 class=xl70 style=width:49pt92a4053/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptDörr et al./td

    td width=593 class=xl70 style=width:445ptForced and internal components

    of observed Arctic sea ice changes/td

    td width=65 class=xl70 style=width:49pt92a4054/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptKolbe et al./td

    td width=593 class=xl70 style=width:445ptExtension of the sea ice climate

    time series with historical satellite data from the 1970s/td

    td width=65 class=xl70 style=width:49pt92a4055/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:15/td

    td width=177 class=xl72 style=width:133ptPirlet et al./td

    td width=593 class=xl70 style=width:445ptHow much does Antarctic landfast

    ice affect coastal polynyas at the circumpolar scale?/td

    td width=65 class=xl70 style=width:49pt92a4056/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptOsanen et al./td

    td width=593 class=xl70 style=width:445ptApplication of an Underwater

    Hyperspectral Imager (UHI) for the study of sea ice algal biomass

    distribution and production/td

    td width=65 class=xl70 style=width:49pt92a4057/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBoutin et al./td

    td width=593 class=xl70 style=width:445ptA coupled ice-ocean framework to

    investigate the impact of sea-ice deformation in the winter sea-ice mass

    balance in the Arctic./td

    td width=65 class=xl70 style=width:49pt92a4058/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLänger et al./td

    td width=593 class=xl70 style=width:445ptA model intercomparison provides

    new insights into carbon cycling in the Canadian Arctic Ocean/td

    td width=65 class=xl70 style=width:49pt92a4059/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptLänger et al./td

    td width=593 class=xl70 style=width:445ptModelling the carbon system in a

    rapidly changing Arctic Ocean/td

    td width=65 class=xl70 style=width:49pt92a4060/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptGranskog et al./td

    td width=593 class=xl70 style=width:445ptNew insights on Arctic sea-ice

    ridges from the MOSAiC expedition - an overview/td

    td width=65 class=xl70 style=width:49pt92a4061/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:45/td

    td width=177 class=xl72 style=width:133ptCheng et al./td

    td width=593 class=xl70 style=width:445ptObservation and modeling of snow

    and land fast sea ice interaction in YoungSound, East Greenland/td

    td width=65 class=xl70 style=width:49pt92a4062/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptHartley et al./td

    td width=593 class=xl70 style=width:445ptIntimate in situ data collection

    over a unique spatiotemporal period - The Last Ice Sentinels Expedition/td

    td width=65 class=xl70 style=width:49pt92a4063/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt9:40/td

    td width=177 class=xl72 style=width:133ptBoutin et al./td

    td width=593 class=xl70 style=width:445ptWave impact on sea ice dynamics

    in the marginal ice zone using a coupled wave—sea-ice model/td

    td width=65 class=xl70 style=width:49pt92a4064/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptGlissenaar et al./td

    td width=593 class=xl70 style=width:445ptTrends and variability from a

    sea ice thickness proxy in the Canadian Arctic (1996-2021)/td

    td width=65 class=xl70 style=width:49pt92a4065/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptTsarau et al./td

    td width=593 class=xl70 style=width:445ptTowards a high-resolution

    multi-scale sea ice model combining continuum and DEM approaches/td

    td width=65 class=xl70 style=width:49pt92a4066/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptSievers et al./td

    td width=593 class=xl70 style=width:445ptAssimilating CryoSat2 freeboard/td

    td width=65 class=xl70 style=width:49pt92a4067/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRedmond Roche et al./td

    td width=593 class=xl70 style=width:445ptCalculations of

    photosynthetically activate radiation transmittance values at the ice-ocean

    interface for varying thicknesses and types of sea ice and snow/td

    td width=65 class=xl70 style=width:49pt92a4068/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptShi et al./td

    td width=593 class=xl70 style=width:445ptDaily snow depth and sea ice

    thickness obtained from the combined CryoSat-2, AVHRR, and AMSR measurements/td

    td width=65 class=xl70 style=width:49pt92a4069/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptNicolaus et al./td

    td width=593 class=xl70 style=width:445ptCharacteristics and composition

    of sea ice in the transpolar drift over the annual cycle/td

    td width=65 class=xl70 style=width:49pt92a4071/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKing et al./td

    td width=593 class=xl70 style=width:445ptEvaluating ACCESS-OM2

    zooplankton biomass estimates using empirical observations/td

    td width=65 class=xl70 style=width:49pt92a4072/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptYe et al./td

    td width=593 class=xl70 style=width:445ptArctic sea ice type distribution

    from various microwave remote sensing products/td

    td width=65 class=xl70 style=width:49pt92a4073/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTian-Kunze et al./td

    td width=593 class=xl70 style=width:445ptTriple Collocation Analysis of

    SMOS-derived Sea-Ice Thickness Products using MODIS, Ocean-Ice Model and ULS

    data/td

    td width=65 class=xl70 style=width:49pt92a4074/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptNeckel et al./td

    td width=593 class=xl70 style=width:445ptTwo+ decades (2000-2023) of pan

    Arctic meltpond fraction data/td

    td width=65 class=xl70 style=width:49pt92a4075/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptMartínez Moreno et al./td

    td width=593 class=xl70 style=width:445ptOcean eddies drive heterogeneity

    in the sea-ice growth/td

    td width=65 class=xl70 style=width:49pt92a4076/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptMaus et al./td

    td width=593 class=xl70 style=width:445ptBounds on the macroporosity of

    sea ice pressure ridges/td

    td width=65 class=xl70 style=width:49pt92a4078/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptSchlindwein et al./td

    td width=593 class=xl70 style=width:445ptSeasonal variations in seismic

    noise emissions of Arctic sea ice recorded by deep-water ocean bottom

    seismometers: implications for ice deformation and swell generation/td

    td width=65 class=xl70 style=width:49pt92a4079/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptMuchow et al./td

    td width=593 class=xl70 style=width:445ptModelling ridging on local

    scales using discrete element methods/td

    td width=65 class=xl70 style=width:49pt92a4080/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptKrumpen et al./td

    td width=593 class=xl70 style=width:445ptInterannual variability and

    trends in Arctic sea ice thickness and surface roughness: Insights from two

    decades of airborne observations/td

    td width=65 class=xl70 style=width:49pt92a4081/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptSticker et al./td

    td width=593 class=xl70 style=width:445ptArctic rapid sea ice loss events

    in models simulations./td

    td width=65 class=xl70 style=width:49pt92a4082/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptXiu et al./td

    td width=593 class=xl70 style=width:445ptSeasonal prediction of NorCPM in

    the regional Antarctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4084/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt9:00/td

    td width=177 class=xl72 style=width:133ptDiamond et al./td

    td width=593 class=xl70 style=width:445ptDo melt-ponds matter? Sea-ice

    parametrisations during three different climate periods/td

    td width=65 class=xl70 style=width:49pt92a4085/td

    /tr

    tr height=37 style=page-break-before:always; height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLessard-Hamel et al./td

    td width=593 class=xl70 style=width:445ptEngineering challenges in the

    development of an in situ microscopic imaging system for sea ice observation./td

    td width=65 class=xl70 style=width:49pt92a4086/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptAylmer et al./td

    td width=593 class=xl70 style=width:445ptModulation of future sea ice

    loss by ocean heat transport/td

    td width=65 class=xl70 style=width:49pt92a4087/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptMelsheimer et al./td

    td width=593 class=xl70 style=width:445ptAntarctic sea ice types with

    active and passive microwave satellite observations: First improvements/td

    td width=65 class=xl70 style=width:49pt92a4088/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:30/td

    td width=177 class=xl72 style=width:133ptMelsheimer et al./td

    td width=593 class=xl70 style=width:445ptSatellite Remote Sensing of Snow

    on Antarctic Sea Ice with Microwave Radiometry/td

    td width=65 class=xl70 style=width:49pt92a4089/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptAylmer et al./td

    td width=593 class=xl70 style=width:445ptSummertime rapid sea ice loss

    events on sub-seasonal timescales/td

    td width=65 class=xl70 style=width:49pt92a4090/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKaidel et al./td

    td width=593 class=xl70 style=width:445ptIn Situ Observations of the

    Thermal Expansion Coefficient of Sea Ice/td

    td width=65 class=xl70 style=width:49pt92a4091/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRichter et al./td

    td width=593 class=xl70 style=width:445ptFrazil ice in CTDs: effects on

    measurements of supercooling/td

    td width=65 class=xl70 style=width:49pt92a4092/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptMeier et al./td

    td width=593 class=xl70 style=width:445ptImproved sea ice drift estimates

    from enhanced-resolution passive microwave data/td

    td width=65 class=xl70 style=width:49pt92a4093/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt9:20/td

    td width=177 class=xl72 style=width:133ptRichter et al./td

    td width=593 class=xl70 style=width:445ptDrivers of interannual fast-ice

    variability in McMurdo Sound: an investigation on multiple scales/td

    td width=65 class=xl70 style=width:49pt92a4094/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptYang et al./td

    td width=593 class=xl70 style=width:445ptThe evolution of the Fram Strait

    sea ice volume export decomposed by age: estimating with parameter-optimized

    sea ice-ocean model outputs/td

    td width=65 class=xl70 style=width:49pt92a4095/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptPerovich et al./td

    td width=593 class=xl70 style=width:445ptSolar heat partitioning at the

    MOSAiC Central Observatory/td

    td width=65 class=xl70 style=width:49pt92a4096/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKrampe et al./td

    td width=593 class=xl70 style=width:445ptChallenges of dedicated snow

    modeling in high latitudes/td

    td width=65 class=xl70 style=width:49pt92a4097/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptCaldarella et al./td

    td width=593 class=xl70 style=width:445ptTowards Quantifying Frazil Ice

    Using Retrievals from an Acoustic Profiler, a Camera and Plume Models/td

    td width=65 class=xl70 style=width:49pt92a4098/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptJahn et al./td

    td width=593 class=xl70 style=width:445ptProjections of a summer ice free

    Arctic: A review of current climate model projections/td

    td width=65 class=xl70 style=width:49pt92a4099/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptJahn et al./td

    td width=593 class=xl70 style=width:445ptFundamental changes in the North

    Water Polynya less likely if warming is limited to 2°C/td

    td width=65 class=xl70 style=width:49pt92a4100/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptMensah et al./td

    td width=593 class=xl70 style=width:445ptA century-long decreasing trend

    in Bering Sea ice melt revealed by T-S-based estimates/td

    td width=65 class=xl70 style=width:49pt92a4101/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptHaas et al./td

    td width=593 class=xl70 style=width:445ptMultisensor observations of sea

    ice melt across the marginal ice zone/td

    td width=65 class=xl70 style=width:49pt92a4102/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMensah et al./td

    td width=593 class=xl70 style=width:445ptTrends in sea ice melt in the

    Labrador Sea and Baffin Bay estimated from spring salinity profiles/td

    td width=65 class=xl70 style=width:49pt92a4103/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:15/td

    td width=177 class=xl72 style=width:133ptHaas et al./td

    td width=593 class=xl70 style=width:445ptThickness of the Berkner Island

    fast ice tongue: Implications for Ice Shelf Water/td

    td width=65 class=xl70 style=width:49pt92a4104/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptSwiggs et al./td

    td width=593 class=xl70 style=width:445ptInvestigating changes in sea ice

    lead density in the Northwest Passage using satellite altimetry and optical

    imagery/td

    td width=65 class=xl70 style=width:49pt92a4105/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptReifenberg et al./td

    td width=593 class=xl70 style=width:445ptObservations of Summer Ice Melt

    and Ice-Ocean Boundary Layer Heat Fluxes in the Marginal Ice Zone North of

    Fram Strait/td

    td width=65 class=xl70 style=width:49pt92a4107/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptHapp et al./td

    td width=593 class=xl70 style=width:445ptEmploying data-science methods

    for mapping sea ice surface change on decadal time scales/td

    td width=65 class=xl70 style=width:49pt92a4108/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptWang et al./td

    td width=593 class=xl70 style=width:445ptThe impacts of combined SAM and

    ENSO on seasonal Antarctic sea ice changes/td

    td width=65 class=xl70 style=width:49pt92a4109/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptZhou et al./td

    td width=593 class=xl70 style=width:445ptSNOW EFFECTS ON CRYOSAT-2

    WAVEFORM OVER SEA ICE IN THE WEDDELL SEA/td

    td width=65 class=xl70 style=width:49pt92a4110/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptSchweiger et al./td

    td width=593 class=xl70 style=width:445ptPolynya Events in the Wandel Sea/td

    td width=65 class=xl70 style=width:49pt92a4111/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptHoppmann et al./td

    td width=593 class=xl70 style=width:445ptUsing distributed observations

    of the coupled Arctic system to capture spatial and temporal variability:

    Example from MOSAiC/td

    td width=65 class=xl70 style=width:49pt92a4113/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFeltham et al./td

    td width=593 class=xl70 style=width:445ptImplementation of internal wave

    drag in the CICE model/td

    td width=65 class=xl70 style=width:49pt92a4114/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt10:00/td

    td width=177 class=xl72 style=width:133ptHaumann et al./td

    td width=593 class=xl70 style=width:445ptAn abrupt transition in

    Antarctic sea ice–ocean system/td

    td width=65 class=xl70 style=width:49pt92a4115/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptMoore et al./td

    td width=593 class=xl70 style=width:445ptEvolving relationship of Nares

    Strait ice arches and the North Water Polynya/td

    td width=65 class=xl70 style=width:49pt92a4116/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMuller et al./td

    td width=593 class=xl70 style=width:445ptMelting-refreezing vs melting

    bags-equilibration method: an intercomparison for gases measurements in sea

    ice/td

    td width=65 class=xl70 style=width:49pt92a4117/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptNicolaus et al./td

    td width=593 class=xl70 style=width:445ptYear-round interdisciplinary

    observations of the under-ice environment using a remotely operated vehicle

    during the Arctic expeditions/td

    td width=65 class=xl70 style=width:49pt92a4118/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptCrabeck et al./td

    td width=593 class=xl70 style=width:445ptThe role of sea ice in the

    carbon budget of Polar Oceans, a decade of work/td

    td width=65 class=xl70 style=width:49pt92a4120/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKimura et al./td

    td width=593 class=xl70 style=width:445ptThe Freshening of the Ocean by

    Melt Pond and Deformation of Sea Ice from Ice-Tethered Buoy/GPS Observations/td

    td width=65 class=xl70 style=width:49pt92a4121/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptMassom et al./td

    td width=593 class=xl70 style=width:445ptChange and variability in

    Antarctic coastal exposure to open-ocean (sea ice-free) conditions since 1979/td

    td width=65 class=xl70 style=width:49pt92a4122/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptJewell et al./td

    td width=593 class=xl70 style=width:445ptAtmospheric drivers of winter

    lead opening in the Beaufort Sea and impacts on large-scale patterns of sea

    ice transport/td

    td width=65 class=xl70 style=width:49pt92a4124/td

    /tr

    tr height=37 style=page-break-before:always; height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBathmann et al./td

    td width=593 class=xl70 style=width:445ptSAR-Based Sea Ice Drift and

    Lagrangian Tracking for Evaluating Sea Ice Drift Forecast Models/td

    td width=65 class=xl70 style=width:49pt92a4125/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptKomatsu et al./td

    td width=593 class=xl70 style=width:445ptMapping of sea-ice melting and

    net freshwater flux by sea-ice growth/melt in the Southern Ocean/td

    td width=65 class=xl70 style=width:49pt92a4126/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptOhshima et al./td

    td width=593 class=xl73 style=width:445ptDominant frazil ice production,

    associated dense water formation and material transport in Antarctic coastal

    polynyas/td

    td width=65 class=xl70 style=width:49pt92a4127/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRusin et al./td

    td width=593 class=xl70 style=width:445ptSea Ice Concentration Retrievals

    from Microwave Radiometry : a New Algorithm for AMSR2/td

    td width=65 class=xl70 style=width:49pt92a4128/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptDown et al./td

    td width=593 class=xl70 style=width:445ptA Climate Data Record of Global

    Sea-Ice Drift from the EUMETSAT OSI SAF/td

    td width=65 class=xl70 style=width:49pt92a4129/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptOhshima et al./td

    td width=593 class=xl70 style=width:445ptLate summer frazil ice formation

    with high Chlorophyll off the Amery Ice Shelf and Cape Darnley/td

    td width=65 class=xl70 style=width:49pt92a4130/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptEdel et al./td

    td width=593 class=xl70 style=width:445ptReconstruction of Arctic sea ice

    thickness (2000-2010) based on a hybrid machine learning and data

    assimilation approach/td

    td width=65 class=xl70 style=width:49pt92a4131/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt9:00/td

    td width=177 class=xl72 style=width:133ptHaas et al./td

    td width=593 class=xl70 style=width:445ptRecent advances in airborne

    surveying of sea ice and snow thickness/td

    td width=65 class=xl70 style=width:49pt92a4132/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptRückert et al./td

    td width=593 class=xl70 style=width:445ptModelling snow and ice microwave

    emissions in the Arctic for a satellite-based water vapor retrieval/td

    td width=65 class=xl70 style=width:49pt92a4133/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFrancis et al./td

    td width=593 class=xl70 style=width:445ptLinking winds with sea ice

    changes in the Southern Ocean over the past centuries/td

    td width=65 class=xl70 style=width:49pt92a4134/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLandy et al./td

    td width=593 class=xl70 style=width:445ptThe Bilateral INTERAAC

    (air-snow-ice-ocean INTERactions transforming Atlantic) Collaboration between

    Norway and China/td

    td width=65 class=xl70 style=width:49pt92a4135/td

    /tr

    tr height=56 style=height:42.0pt

    td height=56 width=52 class=xl71 style=height:42.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptLandy et al./td

    td width=593 class=xl70 style=width:445ptWhat can we learn by comparing

    Arctic winter radar and laser freeboards obtained from CryoSat-2, AltiKa and

    ICESat-2 over the common mission period October 2018 – April 2022?/td

    td width=65 class=xl70 style=width:49pt92a4136/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptSchroeder et al./td

    td width=593 class=xl70 style=width:445ptThe role of ocean heat transport

    from the Atlantic into the Arctic Ocean on sea ice variability/td

    td width=65 class=xl70 style=width:49pt92a4137/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptParard et al./td

    td width=593 class=xl70 style=width:445ptON THE RETRIEVAL OF SEA ICE

    PROPERTIES BY MEANS OF ULTRAWIDE BAND MICROWAVE RADIOMETER/td

    td width=65 class=xl70 style=width:49pt92a4138/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptGranskog et al./td

    td width=593 class=xl70 style=width:445ptRegime shift in Arctic Ocean

    sea-ice thickness/td

    td width=65 class=xl70 style=width:49pt92a4139/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptVälisuo et al./td

    td width=593 class=xl70 style=width:445ptArctic sea ice drift in extended

    range forecasts/td

    td width=65 class=xl70 style=width:49pt92a4140/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptLee et al./td

    td width=593 class=xl70 style=width:445ptEstimating Summer Sea Ice

    Thickness from Satellite Passive Microwave Measurements/td

    td width=65 class=xl70 style=width:49pt92a4141/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFærch et al./td

    td width=593 class=xl70 style=width:445ptTime-series Analysis of SAR

    Backscatter from Icebergs at L-and C-band/td

    td width=65 class=xl70 style=width:49pt92a4142/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMishchenko et al./td

    td width=593 class=xl70 style=width:445ptFeatures of changes in the ice

    cover in the seas of the Russian Arctic/td

    td width=65 class=xl70 style=width:49pt92a4143/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptJohansson et al./td

    td width=593 class=xl70 style=width:445ptSea ice type separation using

    the polarization difference in high resolution C- and L-band SAR images/td

    td width=65 class=xl70 style=width:49pt92a4144/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptÓlason et al./td

    td width=593 class=xl70 style=width:445ptSea-ice deformation in a new

    brittle rheology/td

    td width=65 class=xl70 style=width:49pt92a4145/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl72 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptZhang et al./td

    td width=593 class=xl70 style=width:445ptTowards a high-resolution

    multi-scale sea ice model: exploring the potential of modelling floe-scale

    ice fracture with the Peridynamic method/td

    td width=65 class=xl70 style=width:49pt92a4146/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptFeltham et al./td

    td width=593 class=xl70 style=width:445ptA satellite era reanalysis of

    the Arctic sea ice cover utilising year-round observations of sea ice

    thickness/td

    td width=65 class=xl70 style=width:49pt92a4147/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptKirillov et al./td

    td width=593 class=xl70 style=width:445ptThe role of oceanic heat flux in

    reducing thermodynamic ice growth in Nares Strait and promoting earlier

    collapse of the ice bridge/td

    td width=65 class=xl70 style=width:49pt92a4148/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMatthes et al./td

    td width=593 class=xl70 style=width:445ptUnder-ice PAR levels during

    polar night recorded by autonomous profilers/td

    td width=65 class=xl70 style=width:49pt92a4149/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptSingha et al./td

    td width=593 class=xl70 style=width:445ptSimulated brightness

    temperatures of Arctic sea ice and comparisons with AMSR-2 observations at

    swath level/td

    td width=65 class=xl70 style=width:49pt92a4150/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRaphael et al./td

    td width=593 class=xl70 style=width:445ptA simple method for estimating

    the effective thermal conductivity of snow on Arctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4151/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBach et al./td

    td width=593 class=xl70 style=width:445ptDMSP production, primary

    productivity and community composition in new year sea ice in the Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4152/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptAaboe et al./td

    td width=593 class=xl70 style=width:445ptA New Structure for the Sea Ice

    Essential Climate Variables of the Global Climate Observing System/td

    td width=65 class=xl70 style=width:49pt92a4153/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFisser et al./td

    td width=593 class=xl70 style=width:445ptExamining size estimates of

    small and medium icebergs in the Barents Sea, derived from Sentinel-1 data/td

    td width=65 class=xl70 style=width:49pt92a4154/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptBateson et al./td

    td width=593 class=xl70 style=width:445ptUnderstanding the role of

    mechanical break-up in determining sea ice floe size/td

    td width=65 class=xl70 style=width:49pt92a4155/td

    /tr

    tr height=37 style=page-break-before:always; height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptNeudert et al./td

    td width=593 class=xl70 style=width:445ptRetrieval of sea ice porosity

    evolution during MOSAiC from multifrequency electromagnetic measurements/td

    td width=65 class=xl70 style=width:49pt92a4156/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:30/td

    td width=177 class=xl72 style=width:133ptNeudert et al./td

    td width=593 class=xl70 style=width:445ptIce shelf and ocean influences

    on the sub-ice platelet layer in Atka Bay from electromagnetic induction

    sounding and CTD data/td

    td width=65 class=xl70 style=width:49pt92a4157/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptJensen et al./td

    td width=593 class=xl70 style=width:445ptThe Partitioning Processes of

    Sea Ice Associated Marine Ice Nucleation Particles Impacting the Arctic

    Clouds/td

    td width=65 class=xl70 style=width:49pt92a4158/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptRegan et al./td

    td width=593 class=xl70 style=width:445ptModelling the evolution of

    Arctic multiyear sea ice over 2000-2018/td

    td width=65 class=xl70 style=width:49pt92a4159/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt9:20/td

    td width=177 class=xl72 style=width:133ptTilling et al./td

    td width=593 class=xl70 style=width:445ptImproving Year-round Sea Ice

    Observations by Combining Satellite Altimeters and Novel Techniques/td

    td width=65 class=xl70 style=width:49pt92a4160/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptBabb et al./td

    td width=593 class=xl70 style=width:445ptThe Multiyear Sea Ice Area

    Budget of the Arctic Ocean: Export, Melt, Replenishment and a Recent Plateau/td

    td width=65 class=xl70 style=width:49pt92a4161/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRidley et al./td

    td width=593 class=xl70 style=width:445ptArctic sea ice decline in a

    global climate model results in water vapour, cloud, and boundary layer

    changes/td

    td width=65 class=xl70 style=width:49pt92a4162/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptClemens-Sewall et al./td

    td width=593 class=xl70 style=width:445ptProgress Towards a Single-Column

    Model (Icepack) Case Study for the MOSAiC Expedition/td

    td width=65 class=xl70 style=width:49pt92a4163/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptguo et al./td

    td width=593 class=xl70 style=width:445ptMulti-decadal time series of sea

    ice type classification in the Atlantic sector of the Arctic Ocean retrieved

    from wide-swath Synthetic Aperture Radar data/td

    td width=65 class=xl70 style=width:49pt92a4164/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptWells et al./td

    td width=593 class=xl70 style=width:445ptA mushy model of gas transport

    in porous sea ice/td

    td width=65 class=xl70 style=width:49pt92a4165/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptZhang et al./td

    td width=593 class=xl70 style=width:445ptA year-long mesocosm study of

    weathering processes of microplastics in the sea-ice and ocean environment/td

    td width=65 class=xl70 style=width:49pt92a4166/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptWebster et al./td

    td width=593 class=xl70 style=width:445ptAtmospheric drivers of temporal

    variability in melt pond coverage and albedo:spannbsp;

    /spana model-observation synthesis/td

    td width=65 class=xl70 style=width:49pt92a4167/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptMahmud et al./td

    td width=593 class=xl70 style=width:445ptSea ice monitoring from NISAR/td

    td width=65 class=xl70 style=width:49pt92a4169/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:15/td

    td width=177 class=xl72 style=width:133ptYackel et al./td

    td width=593 class=xl70 style=width:445ptSnow thermo-physical controls on

    X-, C- and L-band SAR backscatter from sea ice: a case study from MOSAiC/td

    td width=65 class=xl70 style=width:49pt92a4170/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:00/td

    td width=177 class=xl72 style=width:133ptChapman-Dutton et al./td

    td width=593 class=xl70 style=width:445ptThe Effects of Late Spring and

    Summer Snowfall on Arctic Sea Ice Radiative Forcing/td

    td width=65 class=xl70 style=width:49pt92a4171/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptYackel et al./td

    td width=593 class=xl70 style=width:445ptSnow depth on landfast sea ice

    in the Canadian Arctic from ICESat-2 and CryoSat-2 and SAR imagery/td

    td width=65 class=xl70 style=width:49pt92a4173/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptFuchs et al./td

    td width=593 class=xl70 style=width:445ptThe overlooked flexibility of

    melt pond bottom ice during formation and drainage – observations and

    implications/td

    td width=65 class=xl70 style=width:49pt92a4174/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptFuchs et al./td

    td width=593 class=xl70 style=width:445ptThe path of light through the

    Arctic sea ice cover/td

    td width=65 class=xl70 style=width:49pt92a4176/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBradley et al./td

    td width=593 class=xl70 style=width:445ptLate summer sea ice extent

    primary driver of summer season coastal erosion rates in Arctic Alaska/td

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    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMacfarlane et al./td

    td width=593 class=xl70 style=width:445ptOcean-sourced snow on Arctic sea

    ice/td

    td width=65 class=xl70 style=width:49pt92a4178/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptDroste et al./td

    td width=593 class=xl70 style=width:445ptThe role of sea ice in the

    interannual variability of sea-air CO2 flux along the West Antarctic

    Peninsula/td

    td width=65 class=xl70 style=width:49pt92a4179/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTsamados et al./td

    td width=593 class=xl70 style=width:445ptHigh-resolution sea ice

    concentration budget analysis in the Arctic’s Last Ice Area/td

    td width=65 class=xl70 style=width:49pt92a4180/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptJutila et al./td

    td width=593 class=xl70 style=width:445ptInsights to seasonal sea-ice

    surface roughness evolution and variability using MOSAiC airborne laser

    scanning/td

    td width=65 class=xl70 style=width:49pt92a4181/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt9:20/td

    td width=177 class=xl72 style=width:133ptScharien et al./td

    td width=593 class=xl70 style=width:445ptSeasonal variations in L-band

    frequency microwave backscatter from Arctic sea ice using surface and

    satellite observations/td

    td width=65 class=xl70 style=width:49pt92a4182/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptScharien et al./td

    td width=593 class=xl70 style=width:445ptThe sea ice phenology explorer

    tool: a publicly accessible tool for exploring landfast sea ice-climate

    indicators/td

    td width=65 class=xl70 style=width:49pt92a4183/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFraser et al./td

    td width=593 class=xl70 style=width:445ptAntarctic landfast sea ice:

    Physical, biogeochemical and ecological significance/td

    td width=65 class=xl70 style=width:49pt92a4184/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFraser et al./td

    td width=593 class=xl70 style=width:445ptThe Emperor’s Smooth Floes; or

    why emperor penguins care about Antarctic fast ice roughness/td

    td width=65 class=xl70 style=width:49pt92a4186/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFraser et al./td

    td width=593 class=xl70 style=width:445ptThe Emperor’s Smooth Floes; or

    why emperor penguins care about Antarctic fast ice roughness/td

    td width=65 class=xl70 style=width:49pt92a4186/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptFraser et al./td

    td width=593 class=xl70 style=width:445ptRemotely-sensing the

    wave-affected Antarctic marginal ice zone using pulse-limited radar

    altimeters/td

    td width=65 class=xl70 style=width:49pt92a4187/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:00/td

    td width=177 class=xl72 style=width:133ptMartin et al./td

    td width=593 class=xl70 style=width:445ptThe influence of snow on

    Antarctic sea ice evolution: Drone-based mapping of the snow surface

    temperature/td

    td width=65 class=xl70 style=width:49pt92a4188/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptSaylam et al./td

    td width=593 class=xl70 style=width:445ptAnalysis of Arctic summer sea

    ice heights to validate ICESat-2 measurements with airborne lidar technology./td

    td width=65 class=xl70 style=width:49pt92a4189/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptYi et al./td

    td width=593 class=xl70 style=width:445ptComparing Cryosat-2 FF-SAR Sea

    Ice Freeboard with Cryosat-2, IceBridge/ATM, and ICESat-2 Freeboards in the

    Arctic/td

    td width=65 class=xl70 style=width:49pt92a4190/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptJoshi et al./td

    td width=593 class=xl70 style=width:445ptSeasonal and inter-annual

    variations in sea ice thickness in the Weddell Sea, Antarctica (2019-2022)

    using ICESat-2/td

    td width=65 class=xl70 style=width:49pt92a4191/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:00/td

    td width=177 class=xl72 style=width:133ptRapp et al./td

    td width=593 class=xl70 style=width:445ptGenomic signatures of transience

    and stability: Microbial adaptations and interactions in first-year and

    multi-year sea ice/td

    td width=65 class=xl70 style=width:49pt92a4192/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptPauling et al./td

    td width=593 class=xl70 style=width:445ptSea Ice Response to Volcanic

    Eruptions in Model Large Ensembles/td

    td width=65 class=xl70 style=width:49pt92a4193/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptPauling et al./td

    td width=593 class=xl70 style=width:445ptSea ice and climate impacts from

    Antarctic ice-mass loss in a multi-model experiment/td

    td width=65 class=xl70 style=width:49pt92a4195/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptChua et al./td

    td width=593 class=xl70 style=width:445ptNilas: A Southern Ocean Mapping

    Platform/td

    td width=65 class=xl70 style=width:49pt92a4196/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptScott et al./td

    td width=593 class=xl70 style=width:445ptSea ice concentration and

    uncertainty estimates using brightness temperatures and atmospheric variables

    with a Bayesian neural network/td

    td width=65 class=xl70 style=width:49pt92a4197/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptWilhelmus et al./td

    td width=593 class=xl70 style=width:445ptA new sea ice drift product for

    optical remote sensing Imagery/td

    td width=65 class=xl70 style=width:49pt92a4198/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptKurtz et al./td

    td width=593 class=xl70 style=width:445ptICESat-2 Mission Status and Sea

    Ice Product Updates/td

    td width=65 class=xl70 style=width:49pt92a4199/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptGupta et al./td

    td width=593 class=xl70 style=width:445ptMesoscale aggregation of sea ice

    floes in the marginal ice zone/td

    td width=65 class=xl70 style=width:49pt92a4200/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptCorkill et al./td

    td width=593 class=xl70 style=width:445ptA novel probe to sample

    trace-metal concentrations in sea ice at high vertical resolution/td

    td width=65 class=xl70 style=width:49pt92a4201/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptGupta et al./td

    td width=593 class=xl70 style=width:445ptThe three-dimensional life cycle

    of sea ice floes in the Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4202/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptHutter et al./td

    td width=593 class=xl70 style=width:445ptMOSAiC airborne laser scanning

    of the sea-ice surface: a year round data product of high-resolution digital

    elevation models/td

    td width=65 class=xl70 style=width:49pt92a4203/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:45/td

    td width=177 class=xl72 style=width:133ptZampieri et al./td

    td width=593 class=xl70 style=width:445ptModeling the sea ice and snow

    heat conduction through the lens of the MOSAiC dataset/td

    td width=65 class=xl70 style=width:49pt92a4204/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptWongpan et al./td

    td width=593 class=xl70 style=width:445ptHelicopter-based ice-covered

    ocean observations capture broad ocean heat intrusions towards the Totten Ice

    Shelf/td

    td width=65 class=xl70 style=width:49pt92a4205/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt9:00/td

    td width=177 class=xl72 style=width:133ptHutter et al./td

    td width=593 class=xl70 style=width:445ptLinking the evolution of

    floe-scale ice characteristics to its deformation history using satellite

    observations/td

    td width=65 class=xl70 style=width:49pt92a4206/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptPreußer et al./td

    td width=593 class=xl70 style=width:445ptSnow and ice thickness derived

    from sea ice mass balance buoys in the Transpolar Drift system/td

    td width=65 class=xl70 style=width:49pt92a4207/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptPreußer et al./td

    td width=593 class=xl70 style=width:445ptImprovement of MODIS-based

    winter sea-ice production estimates in Arctic polynyas by means of a

    model-based temperature adjustment scheme/td

    td width=65 class=xl70 style=width:49pt92a4208/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptLight et al./td

    td width=593 class=xl70 style=width:445ptGrowing sea ice in the lab:

    controlled forcing, sample amendment, and replication for sea ice process

    studies/td

    td width=65 class=xl70 style=width:49pt92a4209/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptWillatt et al./td

    td width=593 class=xl70 style=width:445ptNovel techniques for estimation

    of snow depth over sea ice using the KuKa surface-based, dual-frequency,

    polarimetric radar/td

    td width=65 class=xl70 style=width:49pt92a4210/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptMeier et al./td

    td width=593 class=xl70 style=width:445ptWhat’s Next for the NOAA /NSIDC

    Passive Microwave-Based Sea Ice Concentration Climate Data Record/td

    td width=65 class=xl70 style=width:49pt92a4212/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptDay et al./td

    td width=593 class=xl70 style=width:445ptStatistically classifying the

    pan-Antarctic marginal ice zone with CICE6/td

    td width=65 class=xl70 style=width:49pt92a4213/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptBollmann et al./td

    td width=593 class=xl70 style=width:445ptApproaches to determine the

    surface roughness of Arctic sea ice using a laser scanner onboard the

    helicopter-borne measurement system HELiPOD/td

    td width=65 class=xl70 style=width:49pt92a4214/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptDeschepper et al./td

    td width=593 class=xl70 style=width:445ptSympagic compartment reveals the

    details of primary production dynamics at the scale of Hudson Bay: lessons

    for the present and insights into the near future/td

    td width=65 class=xl70 style=width:49pt92a4215/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptAaboe et al./td

    td width=593 class=xl70 style=width:445ptFour decades of sea ice observed

    from Space: sea ice type and hemispheric distribution/td

    td width=65 class=xl70 style=width:49pt92a4216/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptAaboe et al./td

    td width=593 class=xl70 style=width:445ptRetreating sea ice in the

    Barents Sea - the Arctic Hotspot region/td

    td width=65 class=xl70 style=width:49pt92a4217/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptYang et al./td

    td width=593 class=xl70 style=width:445ptAn ensemble-based Data

    Assimilation System for the Southern Ocean (DASSO)/td

    td width=65 class=xl70 style=width:49pt92a4219/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptGerland et al./td

    td width=593 class=xl70 style=width:445ptMonitoring of landfast sea ice

    at Storfjorden, Svalbard/td

    td width=65 class=xl70 style=width:49pt92a4220/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptSoriot et al./td

    td width=593 class=xl70 style=width:445ptToward 30 Years of Sea Ice

    Thickness and Sea Ice Volume Estimation From Passive Microwave Radiometers

    Observations/td

    td width=65 class=xl70 style=width:49pt92a4221/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptGerland et al./td

    td width=593 class=xl70 style=width:445ptSea ice studies in a changing

    northern Barents Sea within the multidisciplinary Nansen Legacy project/td

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    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTakata-Glushkoff et al./td

    td width=593 class=xl70 style=width:445ptSivuqaq Sea Ice Changes:

    Regional Remote Sensing and Local St. Lawrence Island Yupik Perspectives/td

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    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl72 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptRheinlænder et al./td

    td width=593 class=xl70 style=width:445ptSimulating winter sea-ice

    breakup in the Beaufort Sea from 2000-2018 and its implications for MYI

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    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRückert et al./td

    td width=593 class=xl70 style=width:445ptUsing a rotatable mirror for

    ship-based microwave radiometer measurements of surface emissivity/td

    td width=65 class=xl70 style=width:49pt92a4227/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:15/td

    td width=177 class=xl72 style=width:133ptWollenburg et al./td

    td width=593 class=xl70 style=width:445ptThe importance of sea-ice

    derived cryogenic minerals on ballasting marine algae aggregates in the polar

    oceans/td

    td width=65 class=xl70 style=width:49pt92a4228/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptPhan et al./td

    td width=593 class=xl70 style=width:445ptFracturing ice floes by

    percussion in a granular model/td

    td width=65 class=xl70 style=width:49pt92a4229/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRohde et al./td

    td width=593 class=xl70 style=width:445ptLoRa on Ice: live sea ice

    monitoring with open-source technology/td

    td width=65 class=xl70 style=width:49pt92a4230/td

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    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptMäkynen et al./td

    td width=593 class=xl70 style=width:445ptArctic thin ice detection using

    AMSR2 and FY-3C MWRI radiometer data/td

    td width=65 class=xl70 style=width:49pt92a4231/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKolbe et al./td

    td width=593 class=xl70 style=width:445ptSea and ice surface temperature

    CDR and trends using AVHRR thermal Infrared satellite sensors 1982-2022/td

    td width=65 class=xl70 style=width:49pt92a4232/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptWulf et al./td

    td width=593 class=xl70 style=width:445ptOperational High Resolution

    Arctic Sea Ice Concentration Retrievalspannbsp;

    /spanusing SAR and Passive Microwave Observations/td

    td width=65 class=xl70 style=width:49pt92a4233/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptVeyssiere et al./td

    td width=593 class=xl70 style=width:445ptSea ice surface radiative fluxes

    from ground and airborne observations in the Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4234/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptMehlmann et al./td

    td width=593 class=xl70 style=width:445ptSimulating deformation structure

    in viscous-plastic sea-ice models with CD-grid approaches/td

    td width=65 class=xl70 style=width:49pt92a4235/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTreffeisen et al./td

    td width=593 class=xl70 style=width:445ptPooling Resources to Investigate

    and Share Information on Sea Ice – The SEA ICE PORTAL/td

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    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:00/td

    td width=177 class=xl72 style=width:133ptWongpan et al./td

    td width=593 class=xl70 style=width:445ptModeled Ice Algal Production in

    Antarctic Landfast Sea Ice/td

    td width=65 class=xl70 style=width:49pt92a4237/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptBlockley et al./td

    td width=593 class=xl70 style=width:445ptImpact of Antarctic sea ice

    variability on climate evolution in a CMIP6 model with implications for

    interpretation of future projections/td

    td width=65 class=xl70 style=width:49pt92a4238/td

    /tr

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    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptHaas et al./td

    td width=593 class=xl70 style=width:445ptSea Ice-thickness product

    iNter-comparison eXerciSe – The ESA SIN’XS project/td

    td width=65 class=xl70 style=width:49pt92a4239/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptRicker et al./td

    td width=593 class=xl70 style=width:445ptLinking scales of sea ice

    surface topography: evaluation of ICESat-2 measurements with coincident

    helicopter laser scanning during MOSAiC/td

    td width=65 class=xl70 style=width:49pt92a4241/td

    /tr

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    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptZhang et al./td

    td width=593 class=xl70 style=width:445ptCapacity of the selected CMIP6

    models to simulate Arctic sea ice drift/td

    td width=65 class=xl70 style=width:49pt92a4242/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptScagliola et al./td

    td width=593 class=xl70 style=width:445ptSEA ICE THEMATIC DATA PRODUCTS

    FOR CRISTAL: DESIGN, DEVELOPMENT AND VALIDATION/td

    td width=65 class=xl70 style=width:49pt92a4243/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTaelman et al./td

    td width=593 class=xl70 style=width:445ptTracking individual sea ice

    floes using in-situ ice drift observations/td

    td width=65 class=xl70 style=width:49pt92a4244/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptSalganik et al./td

    td width=593 class=xl70 style=width:445ptDifferential summer melt rates

    of ridge keels and level ice in the Central Arctic Ocean During the MOSAiC

    Expedition/td

    td width=65 class=xl70 style=width:49pt92a4245/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt10:00/td

    td width=177 class=xl72 style=width:133ptKorosov et al./td

    td width=593 class=xl70 style=width:445ptSea Ice Age Climate Data Record/td

    td width=65 class=xl70 style=width:49pt92a4246/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptPradel et al./td

    td width=593 class=xl70 style=width:445ptInvestigating the incorporation

    of micro- and nanoplastics into young artificial sea ice/td

    td width=65 class=xl70 style=width:49pt92a4247/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptScagliola et al./td

    td width=593 class=xl70 style=width:445ptPOLAR THEMATIC DATA PRODUCTS FOR

    CIMR: DESIGN, DEVELOPMENT AND VALIDATION/td

    td width=65 class=xl70 style=width:49pt92a4248/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptLu et al./td

    td width=593 class=xl70 style=width:445ptFracture properties of sea ice

    across spatial and temporal scales/td

    td width=65 class=xl70 style=width:49pt92a4249/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptKorosov et al./td

    td width=593 class=xl70 style=width:445ptImproving short-term sea ice

    predictability using deformation observations/td

    td width=65 class=xl70 style=width:49pt92a4250/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptLudwig et al./td

    td width=593 class=xl70 style=width:445ptSea-ice deformation forecasts

    and their scale dependence from the Sea Ice Drift Forecast Experiment

    (SIDFEx)/td

    td width=65 class=xl70 style=width:49pt92a4251/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptKern et al./td

    td width=593 class=xl70 style=width:445ptComparing ESA’s Sea_Ice_cci

    Nimbus-5 ESMR sea ice concentration product v1.0 with Landsat imagery – first

    results/td

    td width=65 class=xl70 style=width:49pt92a4252/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTurner et al./td

    td width=593 class=xl70 style=width:445pt13 years of CryoSat Quality

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    td width=65 class=xl70 style=width:49pt92a4253/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptSteckling et al./td

    td width=593 class=xl70 style=width:445ptInvestigating the surface energy

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    td width=65 class=xl70 style=width:49pt92a4254/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:45/td

    td width=177 class=xl72 style=width:133ptMerkouriadi et al./td

    td width=593 class=xl70 style=width:445ptQuantifying the effect of

    snow-ice formation on SnowModel-LG snow depth and density product/td

    td width=65 class=xl70 style=width:49pt92a4256/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptUusinoka et al./td

    td width=593 class=xl70 style=width:445ptHigh resolution analysis of sea

    ice deformation during MOSAiC/td

    td width=65 class=xl70 style=width:49pt92a4257/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt9:20/td

    td width=177 class=xl72 style=width:133ptStolla et al./td

    td width=593 class=xl70 style=width:445ptUnderstanding the Intermodel

    Spread of Simulated Arctic September Sea-Ice Sensitivity/td

    td width=65 class=xl70 style=width:49pt92a4258/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptNotz et al./td

    td width=593 class=xl70 style=width:445ptScales apart: from brine pockets

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    td width=65 class=xl70 style=width:49pt92a4259/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptKorosov et al./td

    td width=593 class=xl70 style=width:445ptHow can image anisotropy help

    improving a sea ice model?/td

    td width=65 class=xl70 style=width:49pt92a4260/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBirnbaum et al./td

    td width=593 class=xl70 style=width:445ptAirborne observations of melt

    pond characteristics in different Arctic sea ice regimes/td

    td width=65 class=xl70 style=width:49pt92a4261/td

    /tr

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    td height=19 width=52 class=xl72 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptNotz et al./td

    td width=593 class=xl70 style=width:445ptA unified sea-ice area data

    product/td

    td width=65 class=xl70 style=width:49pt92a4262/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptRicker et al./td

    td width=593 class=xl70 style=width:445ptMeasuring snow depth on sea ice

    using a drone-based snow radar/td

    td width=65 class=xl70 style=width:49pt92a4263/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptCHENG et al./td

    td width=593 class=xl70 style=width:445ptAn extreme case of ice

    composition observed in an Arctic lake, a possible scenario for the Arctic

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    td width=65 class=xl70 style=width:49pt92a4266/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptCarret et al./td

    td width=593 class=xl70 style=width:445ptAdded value of the CRYO2ICE

    project and analysis of sea ice surface roughness in multi frequency

    altimetry/td

    td width=65 class=xl70 style=width:49pt92a4268/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptKutschan et al./td

    td width=593 class=xl70 style=width:445ptIce crystal growth in different

    environments: An approach from micro to macro scales/td

    td width=65 class=xl70 style=width:49pt92a4269/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTao et al./td

    td width=593 class=xl70 style=width:445ptSeasonality of spectral

    radiative fluxes and optical properties of Arctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4270/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:30/td

    td width=177 class=xl72 style=width:133ptFlores et al./td

    td width=593 class=xl70 style=width:445ptSea-ice decline makes

    zooplankton stay deeper for longer/td

    td width=65 class=xl70 style=width:49pt92a4271/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl72 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptKauker et al./td

    td width=593 class=xl70 style=width:445ptModeling the seasonal evolution

    of the ice thickness distribution along the MOSAiC drift/td

    td width=65 class=xl70 style=width:49pt92a4272/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptJohnson et al./td

    td width=593 class=xl70 style=width:445ptMapping Arctic sea ice surface

    roughness with Multi-angle Imaging SpectroRadiometer and ICESat-II/td

    td width=65 class=xl70 style=width:49pt92a4273/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptTao et al./td

    td width=593 class=xl70 style=width:445ptLight availability and

    variability over and under the Arctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4274/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl72 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptLavergne et al./td

    td width=593 class=xl70 style=width:445ptMonitoring of Sea Ice

    Concentration in the polar regions : 40+ years of data from EUMETSAT OSI SAF

    and ESA CCI/td

    td width=65 class=xl70 style=width:49pt92a4275/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptDi Bella et al./td

    td width=593 class=xl70 style=width:445ptCryoSat: Mission status,

    science, and future challenges over the ice-covered oceans/td

    td width=65 class=xl70 style=width:49pt92a4276/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptLawrence et al./td

    td width=593 class=xl70 style=width:445ptAdding the third dimension to

    recent Antarctic sea ice extent variability/td

    td width=65 class=xl70 style=width:49pt92a4277/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTelegina et al./td

    td width=593 class=xl70 style=width:445ptPrediction of sea ice conditions

    using Sentinel-1 imagery and sea ice drift forecast./td

    td width=65 class=xl70 style=width:49pt92a4278/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptSauer et al./td

    td width=593 class=xl70 style=width:445ptDrivers of extreme summer Arctic

    sea ice reductions with rare event simulation methods/td

    td width=65 class=xl70 style=width:49pt92a4279/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptRitschel et al./td

    td width=593 class=xl70 style=width:445ptSeasonal and regional

    sensitivity of Arctic sea ice/td

    td width=65 class=xl70 style=width:49pt92a4280/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptFrew et al./td

    td width=593 class=xl70 style=width:445ptSea Ice Growth, Melt and

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    td width=65 class=xl70 style=width:49pt92a4281/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptDiaz et al./td

    td width=593 class=xl70 style=width:445ptSalinity, temperature, and δ¹⁸O:

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    td width=65 class=xl70 style=width:49pt92a4282/td

    /tr

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:45/td

    td width=177 class=xl72 style=width:133ptBocquet et al./td

    td width=593 class=xl70 style=width:445ptArctic and Antarctic sea ice

    thickness and volume changes during the last 29 years from satellites/td

    td width=65 class=xl70 style=width:49pt92a4283/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt9:40/td

    td width=177 class=xl72 style=width:133ptWang et al./td

    td width=593 class=xl70 style=width:445ptThe Churchill Marine

    Observatory: A new hub for Arctic system studies/td

    td width=65 class=xl70 style=width:49pt92a4284/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:15/td

    td width=177 class=xl72 style=width:133ptPeeken et al./td

    td width=593 class=xl70 style=width:445ptYellow pancakes - sea ice super

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    td width=65 class=xl70 style=width:49pt92a4285/td

    /tr

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    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptItkin et al./td

    td width=593 class=xl70 style=width:445ptNovel methods for assessment of

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    td width=65 class=xl70 style=width:49pt92a4286/td

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptSmith et al./td

    td width=593 class=xl70 style=width:445ptThe vulnerability of Antarctic

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    td width=65 class=xl70 style=width:49pt92a4287/td

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    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptItkin et al./td

    td width=593 class=xl70 style=width:445ptCombining observational data

    with numerical models for high resolution snow and ice mass balance studies/td

    td width=65 class=xl70 style=width:49pt92a4288/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt17:00/td

    td width=177 class=xl72 style=width:133ptFlintrop et al./td

    td width=593 class=xl70 style=width:445ptCryogenic vs. biogenic

    ballasting of sinking particles in the Southern ocean- implications for

    future carbon export/td

    td width=65 class=xl70 style=width:49pt92a4290/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptMurashkin et al./td

    td width=593 class=xl70 style=width:445ptImproved lead detection with

    Sentinel-1 SAR images in the Arctic/td

    td width=65 class=xl70 style=width:49pt92a4291/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptThomas et al./td

    td width=593 class=xl70 style=width:445ptChemical transport in sea ice: a

    case study/td

    td width=65 class=xl70 style=width:49pt92a4292/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptWieringa et al./td

    td width=593 class=xl70 style=width:445ptBounded and categorized: data

    assimilation in a single-column sea-ice model/td

    td width=65 class=xl70 style=width:49pt92a4293/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptThomas et al./td

    td width=593 class=xl70 style=width:445ptFuture response of Antarctic

    continental shelf properties to ice sheet melting and calving/td

    td width=65 class=xl70 style=width:49pt92a4294/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptPolcwiartek et al./td

    td width=593 class=xl70 style=width:445ptUptake and Fate of Polycyclic

    Aromatic Hydrocarbons in Experimental Sea Ice/td

    td width=65 class=xl70 style=width:49pt92a4295/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptPiras et al./td

    td width=593 class=xl70 style=width:445ptA new time series of altimetric

    data from 1991 to 2012: Benefits of the reprocessing of ERS-1, ERS-2 and

    ENVISAT missions for the sea-ice community/td

    td width=65 class=xl70 style=width:49pt92a4296/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptTsamados et al./td

    td width=593 class=xl70 style=width:445ptWinter and summer Arctic

    observational sea-ice volume budget from CryoSat2 and Polar Pathfinder data

    2011-2020/td

    td width=65 class=xl70 style=width:49pt92a4298/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:00/td

    td width=177 class=xl72 style=width:133ptHimmich et al./td

    td width=593 class=xl70 style=width:445ptUnderstanding recent changes in

    Antarctic sea ice seasonality/td

    td width=65 class=xl70 style=width:49pt92a4299/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptChen et al./td

    td width=593 class=xl70 style=width:445ptTracking Summer Arctic Sea-Ice

    Extent Using Microseism Observation/td

    td width=65 class=xl70 style=width:49pt92a4300/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptMacdonald et al./td

    td width=593 class=xl70 style=width:445ptAssessing sea ice surface

    roughness and elevation in the Canadian Arctic Archipelago using synthetic

    aperture radar (SAR)/td

    td width=65 class=xl70 style=width:49pt92a4301/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptBoulard et al./td

    td width=593 class=xl70 style=width:445ptAdvances in homogeneous time

    series of sea ice thickness and snow depth observed by altimetry/td

    td width=65 class=xl70 style=width:49pt92a4302/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptVancoppenolle et al./td

    td width=593 class=xl70 style=width:445ptInsights on the role of

    cryospheric iron on Southern Ocean phytoplankton phenology from global

    ice-ocean model simulations/td

    td width=65 class=xl70 style=width:49pt92a4303/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptGabriel et al./td

    td width=593 class=xl70 style=width:445ptOptical instrument for in situ

    measurement of the nutrients in sea ice/td

    td width=65 class=xl70 style=width:49pt92a4304/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTedesco et al./td

    td width=593 class=xl73 style=width:445ptSea ice: An extraordinary and

    unique, yet fragile, biome/td

    td width=65 class=xl70 style=width:49pt92a4306/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt12:15/td

    td width=177 class=xl72 style=width:133ptSkourup et al./td

    td width=593 class=xl70 style=width:445ptTowards new Cal/Val Fiducial

    Reference Measurements (FRMs) for Copernicus Sentinel-3 Surface Topography

    Mission – the ESA st3TART project/td

    td width=65 class=xl70 style=width:49pt92a4307/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt10:00/td

    td width=177 class=xl72 style=width:133ptVancoppenolle et al./td

    td width=593 class=xl70 style=width:445ptWhat governs the key transitions

    in the sea ice seasonal cycle?/td

    td width=65 class=xl70 style=width:49pt92a4308/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptVancoppenolle et al./td

    td width=593 class=xl70 style=width:445ptLight Under Arctic Sea Ice in

    Observations and Earth System Models/td

    td width=65 class=xl70 style=width:49pt92a4309/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptPaul et al./td

    td width=593 class=xl70 style=width:445ptThe ESA CCI sea-ice thickness

    CDR: Current state and evolutions/td

    td width=65 class=xl70 style=width:49pt92a4310/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptWillatt et al./td

    td width=593 class=xl70 style=width:445ptDeployment of a surface-based

    Ku- and Ka-band fully polarimetric radar over Antarctic sea ice in the

    Weddell Sea/td

    td width=65 class=xl70 style=width:49pt92a4311/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt13:30/td

    td width=177 class=xl72 style=width:133ptRicker et al./td

    td width=593 class=xl70 style=width:445ptDaily drift-aware sea ice

    freeboard and thickness maps from satellite altimetry/td

    td width=65 class=xl70 style=width:49pt92a4313/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptOttaviani et al./td

    td width=593 class=xl70 style=width:445ptCorrelations between sea ice and

    cloud properties over the Arctic from advanced radiation datasets/td

    td width=65 class=xl70 style=width:49pt92a4314/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptButh et al./td

    td width=593 class=xl70 style=width:445ptLinked observations of melt pond

    properties and sea ice characteristics from aircraft campaigns in the Arctic/td

    td width=65 class=xl73 style=width:49pt92a4315/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptWebster et al./td

    td width=593 class=xl70 style=width:445ptThe Effects of the Arctic

    Oscillation on Snow on Sea Ice in a Warming Arctic/td

    td width=65 class=xl70 style=width:49pt92a4316/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptHerman et al./td

    td width=593 class=xl70 style=width:445ptFrazil ice–waves interactions in

    coastal polynyas/td

    td width=65 class=xl70 style=width:49pt92a4317/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptIstomina et al./td

    td width=593 class=xl70 style=width:445ptArctic and Antarctic summer sea

    ice albedo trends from ENVISAT and Sentinel-3 satellite data/td

    td width=65 class=xl70 style=width:49pt92a4319/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTedesco et al./td

    td width=593 class=xl70 style=width:445ptLink, sink, and return: A new

    sympagic-pelagic-benthic configuration of the Biogeochemical Flux Model/td

    td width=65 class=xl70 style=width:49pt92a4320/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptWed/td

    td width=61 class=xl68 style=width:46pt11:45/td

    td width=177 class=xl72 style=width:133ptKacimi et al./td

    td width=593 class=xl70 style=width:445ptInterannual variability of

    Antarctic snow depth, ice thickness and volume from ICESat-2 and CryoSat-2:

    2019-2022/td

    td width=65 class=xl70 style=width:49pt92a4321/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt15:45/td

    td width=177 class=xl72 style=width:133ptMahoney et al./td

    td width=593 class=xl70 style=width:445ptAlaska landfast ice breakouts:

    large scale risk factors and early warnings/td

    td width=65 class=xl70 style=width:49pt92a4322/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptIstomina et al./td

    td width=593 class=xl70 style=width:445ptRetrieval of summer sea ice

    thickness using melt pond optical properties from satellite data/td

    td width=65 class=xl70 style=width:49pt92a4323/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptStefels et al./td

    td width=593 class=xl70 style=width:445ptDMS(O/P) distribution and

    conversion processes in sympagic and pelagic ecosystems – results from the

    MOSAiC expedition/td

    td width=65 class=xl70 style=width:49pt92a4324/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptBoisvert et al./td

    td width=593 class=xl70 style=width:445ptTiming of Rainfall Associated

    with Arctic Cyclones and Impacts on the Sea Ice/td

    td width=65 class=xl70 style=width:49pt92a4325/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:15/td

    td width=177 class=xl72 style=width:133ptCapelli et al./td

    td width=593 class=xl70 style=width:445ptDeveloping an unmanned airborne

    electromagnetic system for sea ice and snow thickness measurements/td

    td width=65 class=xl70 style=width:49pt92a4326/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptDeRepentigny et al./td

    td width=593 class=xl70 style=width:445ptThe role of forcing in the

    simulated rate of Arctic sea ice loss/td

    td width=65 class=xl70 style=width:49pt92a4327/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptEinhorn et al./td

    td width=593 class=xl70 style=width:445ptUsing Interferometry to Classify

    Landfast Sea Ice Extent and Stability Along the Outer Alaska Continental

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    td width=65 class=xl70 style=width:49pt92a4328/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptFri/td

    td width=61 class=xl68 style=width:46pt14:15/td

    td width=177 class=xl72 style=width:133ptMaksym et al./td

    td width=593 class=xl70 style=width:445ptThe seasonal evolution of

    Antarctic snow and sea ice thickness from ICESat-2/td

    td width=65 class=xl70 style=width:49pt92a4329/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt16:15/td

    td width=177 class=xl72 style=width:133ptDadic et al./td

    td width=593 class=xl70 style=width:445ptThe Influence of Snow on

    Antarctic Sea Ice/td

    td width=65 class=xl70 style=width:49pt92a4330/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFedders et al./td

    td width=593 class=xl70 style=width:445ptTwo-dimensional thermal and

    dynamical strain in landfast sea ice from InSAR: results from a new

    analytical inverse method and field observations/td

    td width=65 class=xl70 style=width:49pt92a4331/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptDuncan et al./td

    td width=593 class=xl70 style=width:445ptThe seasonal evolution of sea

    ice deformation in the Arctic and Southern Oceans/td

    td width=65 class=xl70 style=width:49pt92a4332/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt14:30/td

    td width=177 class=xl72 style=width:133ptGoessling et al./td

    td width=593 class=xl70 style=width:445ptTowards seamless sea-ice

    prediction at AWI with global models and ensemble data assimilation/td

    td width=65 class=xl70 style=width:49pt92a4333/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt14:00/td

    td width=177 class=xl72 style=width:133ptPolashenski et al./td

    td width=593 class=xl70 style=width:445ptThe Sea Ice Dynamics Experiment

    (SIDEx); Observing Stress-Strain-Fracture in Sea Ice at Floe Scale/td

    td width=65 class=xl70 style=width:49pt92a4334/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptTomar et al./td

    td width=593 class=xl70 style=width:445ptKu-, X- and C-band radar

    backscatter of snow-covered first-year sea ice from surface-based

    scatterometer observations and SMRT simulations/td

    td width=65 class=xl70 style=width:49pt92a4335/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt12:00/td

    td width=177 class=xl72 style=width:133ptLaliberté et al./td

    td width=593 class=xl70 style=width:445ptSatellite-derived under-ice

    photosynthetically available radiation at ice-covered Green Edge ice camp/td

    td width=65 class=xl70 style=width:49pt92a4336/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptChaudhary et al./td

    td width=593 class=xl70 style=width:445ptMapping landfast sea ice

    stability of Canadian Arctic communities using Sentinel-1 SAR between

    2016-2023/td

    td width=65 class=xl70 style=width:49pt92a4337/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptBradley et al./td

    td width=593 class=xl70 style=width:445ptObserved sea ice freeze-up and

    melt dates show robust summer water temperature and weaker winter ice

    thickness feedbacks/td

    td width=65 class=xl70 style=width:49pt92a4338/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt11:30/td

    td width=177 class=xl72 style=width:133ptRaulier et al./td

    td width=593 class=xl70 style=width:445ptRadiative transfer in sea ice:

    from in-ice angular radiance distributions to optical properties/td

    td width=65 class=xl70 style=width:49pt92a4339/td

    /tr

    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptMon/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptFlatland et al./td

    td width=593 class=xl70 style=width:445ptSea ice drift patterns in a

    changing Arctic environment/td

    td width=65 class=xl70 style=width:49pt92a4340/td

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    tr height=19 style=height:14.0pt

    td height=19 width=52 class=xl71 style=height:14.0pt; width:39ptThu/td

    td width=61 class=xl68 style=width:46pt9:40/td

    td width=177 class=xl72 style=width:133ptPolashenski et al./td

    td width=593 class=xl70 style=width:445ptSea Ice Challenge Problems/td

    td width=65 class=xl70 style=width:49pt92a4341/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt15:30/td

    td width=177 class=xl72 style=width:133ptSaha et al./td

    td width=593 class=xl70 style=width:445ptRetrieval of Snow depth over

    Arctic Sea Ice and Lake Ice from Ku- and Ka-band polarimetric radar altimetry/td

    td width=65 class=xl70 style=width:49pt92a4342/td

    /tr

    tr height=37 style=height:28.0pt

    td height=37 width=52 class=xl71 style=height:28.0pt; width:39ptTue/td

    td width=61 class=xl68 style=width:46pt13:45/td

    td width=177 class=xl72 style=width:133ptHoeyer et al./td

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