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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col width=593 style=width:445pt /
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/colgrouptbodytr height=28 style=height:21.0pt
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
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:46pt13:45/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
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:46pt14:45/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
td width=65 class=xl70 style=width:49pt92a4177/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: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
td width=65 class=xl70 style=width:49pt92a4224/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: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
td width=65 class=xl70 style=width:49pt92a4225/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:46pt14:30/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
transport/td
td width=65 class=xl70 style=width:49pt92a4226/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: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
/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: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
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: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
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: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
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:46pt14:15/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
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: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
td width=65 class=xl70 style=width:49pt92a4236/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: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
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: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
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: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
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: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
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:46pt14:00/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
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: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
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: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
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: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
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: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
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: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
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: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
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: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
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:133ptTurner et al./td
td width=593 class=xl70 style=width:445pt13 years of CryoSat Quality
Control: Evolution and Current Status of the Ice Processors/td
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
balance at the Arctic sea-ice edge/td
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
to global climate/td
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
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:46pt14:30/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
land-fast sea ice in the future?spannbsp;/span/td
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
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: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
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: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
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: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
Dynamics in an Increasingly Marginal Arctic/td
td width=65 class=xl70 style=width:49pt92a4281/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:133ptDiaz et al./td
td width=593 class=xl70 style=width:445ptSalinity, temperature, and δ¹⁸O:
making sense of the record in sea ice/td
td width=65 class=xl70 style=width:49pt92a4282/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:46pt14:45/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
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: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
bloom in the south-eastern Weddell Sea/td
td width=65 class=xl70 style=width:49pt92a4285/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:133ptItkin et al./td
td width=593 class=xl70 style=width:445ptNovel methods for assessment of
sea ice cover from SAR-derived deformation/td
td width=65 class=xl70 style=width:49pt92a4286/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:133ptSmith et al./td
td width=593 class=xl70 style=width:445ptThe vulnerability of Antarctic
last-fast sea ice to winter storms: lessons from McMurdo Sound in 2019 and
2022/td
td width=65 class=xl70 style=width:49pt92a4287/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:46pt11:45/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
Shelf/td
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
/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:46pt9:40/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
td width=593 class=xl70 style=width:445ptA satellite climate data record
of sea ice surface temperatures for the Arctic Ocean, 1982-2021/td
td width=65 class=xl70 style=width:49pt92a4343/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:133ptNiehaus et al./td
td width=593 class=xl70 style=width:445ptFrom regional to Arctic-wide
melt pond fraction estimates/td
td width=65 class=xl70 style=width:49pt92a4344/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:133ptSmith et al./td
td width=593 class=xl70 style=width:445ptSunlight in sea ice: competing
effects on the trend towards an increasingly transmissive Arctic summer sea
ice cover/td
td width=65 class=xl70 style=width:49pt92a4345/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:133ptStroeve et al./td
td width=593 class=xl70 style=width:445ptMapping potential timing of
under-ice algal blooms from satellite/td
td width=65 class=xl70 style=width:49pt92a4346/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:133ptFarrell et al./td
td width=593 class=xl70 style=width:445ptAssessing Sea Ice Lead
Characteristics with ICESat-2/td
td width=65 class=xl70 style=width:49pt92a4347/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:133ptSelyuzhenok et al./td
td width=593 class=xl70 style=width:445ptThe bimodality of the East
Siberian fast ice extent: Mechanisms and changes/td
td width=65 class=xl70 style=width:49pt92a4349/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:133ptHaapala et al./td
td width=593 class=xl70 style=width:445ptAnatomy of the MOSAiC sea ice
deformation events/td
td width=65 class=xl70 style=width:49pt92a4350/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:133ptHolt et al./td
td width=593 class=xl70 style=width:445ptUpdates and Analysis of the
On-Ice Arctic Sea Ice Thickness Archive/td
td width=65 class=xl70 style=width:49pt92a4352/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:133ptMohammadi-Aragh et al./td
td width=593 class=xl70 style=width:445ptDeveloping the Arctic Sea Ice
attribution System: the role of snow depth data assimilation/td
td width=65 class=xl70 style=width:49pt92a4353/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:133ptWietz et al./td
td width=593 class=xl70 style=width:445ptSea-ice cover and polar water
masses: implications for bacterial community dynamics, functional ecology,
and ice-seawater connectivity/td
td width=65 class=xl70 style=width:49pt92a4354/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:46pt16:45/td
td width=177 class=xl72 style=width:133ptWietz et al./td
td width=593 class=xl70 style=width:445ptSea-ice cover and polar water
masses: implications for bacterial community dynamics, functional ecology,
and ice-seawater connectivity/td
td width=65 class=xl70 style=width:49pt92a4354/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:133ptHuntemann et al./td
td width=593 class=xl70 style=width:445ptRelation of passive microwave
L-band signal to sea ice physical properties during ice growth phase/td
td width=65 class=xl70 style=width:49pt92a4355/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:133ptDadic et al./td
td width=593 class=xl70 style=width:445ptLandfast sea ice monitoring in
McMurdo Sound using snow profile temperatures and thermistor-string-based ice
mass balance buoys/td
td width=65 class=xl70 style=width:49pt92a4356/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:46pt11:00/td
td width=177 class=xl72 style=width:133ptSpreen et al./td
td width=593 class=xl70 style=width:445ptMicrowave emission of snow and
sea ice during the MOSAiC expedition/td
td width=65 class=xl70 style=width:49pt92a4357/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:46pt14:00/td
td width=177 class=xl72 style=width:133ptFarrell et al./td
td width=593 class=xl70 style=width:445ptExamining the Evolution of Ice
Thickness and Roughness with ICESat-2/td
td width=65 class=xl70 style=width:49pt92a4358/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:133ptSalganik et al./td
td width=593 class=xl70 style=width:445ptSnow refreeze as one of the
mechanisms of Artic sea ice ridge consolidation/td
td width=65 class=xl70 style=width:49pt92a4360/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:133ptRichter et al./td
td width=593 class=xl70 style=width:445ptneXtSIM-DG - A next generation
discontinuous Galerkin sea ice model/td
td width=65 class=xl70 style=width:49pt92a4361/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:133ptNelson et al./td
td width=593 class=xl70 style=width:445ptA single-satellite, combined
active-passive microwave approach to deriving estimates of sea ice thickness/td
td width=65 class=xl70 style=width:49pt92a4362/td
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td width=61 class=xl68 style=width:46pt14:00/td
td width=177 class=xl72 style=width:133ptHeil et al./td
td width=593 class=xl70 style=width:445ptKinematic effects of sea-ice
breakup/td
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td width=61 class=xl68 style=width:46pt12:15/td
td width=177 class=xl72 style=width:133ptHeil et al./td
td width=593 class=xl70 style=width:445ptImpacts of recent Antarctic
Sea-Ice Extremes/td
td width=65 class=xl70 style=width:49pt92a4366/td
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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:445ptCIRFA cruise 2022: a ship-based
Arctic research expedition with focus on satellite remote sensing of floating
ice/td
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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:445ptFuture Projection of Ice-Algal
Production in the Arctic Ocean: Model Intercomparison/td
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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:133ptOggier et al./td
td width=593 class=xl70 style=width:445ptColors of the Arctic - mapping
the evolution of sea ice texture and stratigraphy from first- year to
second-year ice/td
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td width=177 class=xl72 style=width:133ptFredensborg Hansen et al./td
td width=593 class=xl70 style=width:445ptCRYO2ICE under-flight: first
results of sea ice and snow characteristics on Antarctic sea ice from
near-coincident space- and airborne multi-frequency altimetry/td
td width=65 class=xl70 style=width:49pt92a4421/td
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td width=177 class=xl72 style=width:133ptPrice et al./td
td width=593 class=xl70 style=width:445ptSea Ice Thickness in the Western
Ross Sea/td
td width=65 class=xl70 style=width:49pt92a4422/td
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td width=177 class=xl72 style=width:133ptHernandez-Macia-Her/td
td width=593 class=xl70 style=width:445ptMOSAIC L-band microwave models
and measurements comparison to improve the sea ice thickness satellite
measurements/td
td width=65 class=xl70 style=width:49pt92a4423/td
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td width=61 class=xl68 style=width:46pt9:00/td
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td width=593 class=xl70 style=width:445ptWelcome/td
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td width=593 class=xl70 style=width:445ptExcursion information/td
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td width=593 class=xl70 style=width:445ptClosure/td
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