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Impact of sea ice transport on Beaufort Gyre liquid freshwater content
The Arctic Ocean’s Beaufort Gyre (BG) is a wind-driven reservoir of relatively fresh seawater, situated beneath time-mean anticyclonic atmospheric...
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A Cross-Seasonal Linkage between Arctic Sea Ice and Eurasian Summertime Temperature Fluctuations
This study explores the linkage between summertime temperature fluctuations over midlatitude Eurasia and the preceding Arctic sea ice concentration...
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Evaluating Parameterizations for Turbulent Fluxes over the Landfast Sea-Ice Surface in Prydz Bay, Antarctica
It is crucial to appropriately determine turbulent fluxes in numerical models. Using data collected in East Antarctica from 8 April to 26 November...
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Dominant role of early winter Barents–Kara sea ice extent anomalies in subsequent atmospheric circulation changes in CMIP6 models
The mid-latitude climate responses to Arctic sea ice loss remain unclear, partly because the atmospheric responses depend sensitively to the location...
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Effect of compressive strength on the performance of the NEMO-LIM model in Arctic Sea ice simulation
Satellite records show that the extent and thickness of sea ice in the Arctic Ocean have significantly decreased since the early 1970s. The...
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Impact of Arctic Oscillation on cloud radiative forcing and September sea ice retreat
The Arctic Oscillation (AO) has important effects on the sea ice change in terms of the dynamic and thermodynamic processes. However, while the...
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Uncertainties of Drag Coefficient Estimates Above Sea Ice from Field Data
Surface turbulent exchanges play a key role on sea ice dynamics, on ocean and sea ice heat budgets and on the polar atmosphere. Uncertainties in...
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Potential effects of the projected Antarctic sea-ice loss on the climate system
Climate models project that a reduction in the Antarctic sea-ice extent due to global warming in the future would exert an influential role on the...
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Recent strengthening of snow and ice albedo feedback driven by Antarctic sea-ice loss
The decline of the Arctic cryosphere during recent decades has lowered the region’s surface albedo, reducing its ability to reflect solar radiation...
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An improved algorithm for retrieving thin sea ice thickness in the Arctic Ocean from SMOS and SMAP L-band radiometer data
The aim of this study was to develop an improved thin sea ice thickness (SIT) retrieval algorithm in the Arctic Ocean from the Soil Moisture Ocean...
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Role of atmospheric heat fluxes and ocean advection on decadal (2000–2019) change of sea-ice in the Arctic
In this article, role of ocean advection and atmospheric heat fluxes on recent decadal (2000–2019) decrease of sea-ice in the Arctic (60
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Influence of Arctic Sea-ice Concentration on Extended-range Forecasting of Cold Events in East Asia
Utilizing the Community Atmosphere Model, version 4, the influence of Arctic sea-ice concentration (SIC) on the extended-range prediction of three...
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Seasonally distinct contributions of greenhouse gases and anthropogenic aerosols to historical changes in Arctic moisture budget
Arctic hydrological cycle has important global implications through modifying deep ocean circulation via fresh water fluxes. However, attribution of...
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Record-breaking Barents Sea ice loss favors to the unprecedented summertime extreme heatwave in 2021 over western North America by enhancing Rossby wave ridge
A record-setting extreme heatwave occurred over western North America (WNA) in the summer of 2021, which was associated with an extreme atmospheric...
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A Package of Momentum and Heat Transfer Coefficients for the Stable Surface Layer Extended by New Coefficients over Sea Ice
The bulk transfer coefficients of momentum, heat, and humidity belong to the main ingredients of numerical weather prediction and climate models....
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Effects of ocean mesoscale eddies on atmosphere–sea ice–ocean interactions off Adélie Land, East Antarctica
Heat and momentum exchanges at the Southern Ocean surface are crucial for the Earth’s Climate, but the importance of the small-scale spatial...
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Asymmetry in the seasonal cycle of Antarctic sea ice driven by insolation
The mean seasonal cycle of Antarctic sea-ice extent is asymmetric, with the period of ice retreat being approximately two months shorter than the...
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Validation of key Arctic energy and water budget components in CMIP6
We investigate historical simulations of relevant components of the Arctic energy and water budgets for 39 Coupled Model Intercomparison Project...
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Impacts of Arctic sea ice loss on global ocean circulations and interbasin ocean heat exchanges
The Arctic sea ice loss during the past several decades plays an important role in driving global climate change. Herein we explore the effects of...