About Our Analyses

About Our Analyses

As the frozen parts of our planet face rapid and unprecedented change, NSIDC has been sharing how and why its key features are changing. Through accessible visuals and summaries, NSIDC shares current conditions across snow, ice sheets, and sea ice—key components of the global climate system.

NSIDC produces Sea Ice Today, Ice Sheets Today, and Snow Today to serve educators, scientists, stakeholders, policymakers, journalists, and the public. These resources use NASA- and NOAA-funded data to provide timely information and easy-to-interpret graphics on the state of Earth’s cryosphere.

Sea Ice Today 

The Arctic is warming faster than anywhere else on the planet, and as a result, sea ice in the Arctic Ocean is decreasing. Sea ice loss has far-reaching effects on the planet because the ice helps regulate Earth’s climate, influences global weather patterns, and affects ocean circulations. Sea Ice Today provides daily near-real-time data images of Arctic and Antarctic sea ice conditions. Each year, NSIDC scientists also report out the sea ice maximum and minimum.

Sea Ice Today also includes a rich two-decade archive of monthly analyses written by scientists studying changing sea ice conditions and what influences its behavior in both polar regions. Analyses are based on NASA and National Oceanic and Atmospheric Administration (NOAA) data that are freely available to the public through the NASA NSIDC Distributed Active Archive Center. Sea ice analysis posts generally include information on air temperature, pressure, precipitation patterns, circulation patterns, ocean temperatures, and new scientific research from the Arctic science community. The site was formerly known as Arctic Sea Ice News & Analysis (ASINA) before 2024. The analysis archive spans 2006-2025 when funding ended.

Ice Sheets Today

Together, the Antarctic and Greenland Ice Sheets contain more than 99 percent of freshwater ice on Earth. If they both completely melted, they would raise sea level by an estimated 67.4 meters (223 feet). Long-term satellite data indicate that through most of the twentieth century, the ice sheets made very little contribution to sea level, and were nearly in balance in annual snowfall gain and ice or meltwater loss. However, the stability of the ice sheets has changed considerably in the twenty-first century.

Ice Sheets Today provides near-real time maps and graphs of melt conditions on the Greenland Ice Sheet during the melt season, roughly April 1 through November 1. NSIDC scientists, in collaboration with an international team of scientists, report on Greenland Ice Sheet conditions. During the Antarctic melt season,  typically November 1 through April 1, the team publishes periodic maps and graphs of Antarctic Ice Sheet melt conditions. Ice Sheets Today is funded by NASA under the ASINA grant. It was formerly known as Greenland Ice Sheet Today and Antarctic Ice Sheet Today before 2023.

Ice Sheets Today also includes a decade of periodic scientific analyses on surface melting of the Greenland Ice Sheet in the Northern Hemisphere and Antarctic Ice Sheet in the Southern Hemisphere. These articles span the years 2015-2025 when funding ended. 

Snow Today

According to the United States Geological Survey, as much as 75 percent of the water in some western states are derived from snowmelt. Therefore, it is important to track where snow falls and accumulates, to know how much water is stored in snow, and how much solar energy is reflected off clean snow or absorbed by dirty snow, affecting meltwater timing.      

Snow Today website provides daily data images of snow conditions in near real time across the western United States using a combination of satellite data and surface observations. The Snow Today project also provides data and analysis of snow trends across the current season and between seasons. Data and analysis include snow-covered area, snow cover days, how much water is stored in snow (snow water equivalent), snow albedo (the brightness of snow), snow radiative forcing (which measures how much the snow absorbs solar energy because of snow impurities such as dust, dirt, or soot), how recent storms or melt events affect these factors, and how the numbers compare to past years. NASA also funds Snow Today, which is operated in collaboration with the Institute of Arctic and Alpine Research