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Sources of seasonal sea-ice bias for CMIP6 models in the Hudson Bay Complex Publication
Themes: Cryosphere
The seasonal ice-free period in the Hudson Bay Complex (HBC) has grown longer in recent decades in response to warming, both from progressively earlier sea-ice retreat in summer... Read more -
CMIP6 Hudson Bay Sea Ice Thickness Phenology Dataset
Themes: Cryosphere
The seasonal timing of when sea ice thickness falls below ("retreat day") or rises above ("advance day") 10 cm throughout the Northern Hemisphere, based on daily sea ice... Read more -
Bias-corrected CMIP6 Daily Sea Ice Concentration in the Barents and Kara Seas Dataset
Themes: Cryosphere
Daily sea ice concentration (1950 - 2050) from models participating in version 6 of the Coupled Model Intercomparison Project is reprojected to the WGS84/NSIDC 25-km North Polar... Read more -
Climate Forcing of Arctic Sea Ice: Drivers and Impacts Project
Themes: Atmosphere, Cryosphere, Remote Sensing
Canada 150 Chair Professor Julienne Stroeve and her team investigate extreme events in the Arctic and impacts on communities. Research interests and expertise include sea ice... Read more -
Arctic Sea Ice Phenology in CMIP6 Dataset
Themes: Cryosphere
The seasonal timing of summer sea ice retreat (sea ice concentration falls below 15%) and fall sea ice advance (sea ice concentration rises above 15%) is recorded annually, as... Read more -
Arctic Sea Ice Phenology from Passive Microwave Satellite Retrievals Dataset
Themes: Cryosphere
The seasonal timing of summer sea ice opening (sea ice contraction falls below 80%) and retreat (sea ice concentration falls below 15%), as well as fall sea ice advance (sea ice... Read more -
Arctic open-water periods are projected to lengthen dramatically by 2100 Publication
Themes: Cryosphere
The shrinking of Arctic-wide September sea ice extent is often cited as an indicator of modern climate change; however, the timing of seasonal sea ice retreat/advance and the... Read more -
Arctic Sea Ice Phenology Project
Themes: Cryosphere
The annual timing of sea ice retreat and advance throughout seasonally ice-covered seas of the Northern Hemisphere.