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These articles provide answers to frequently asked questions related to Earth's frozen realms. Questions range from general background information and detailed science processes to the data gathered and archived at the National Snow and Ice Data Center (NSIDC) and its data management programs including NOAA@NSIDC, the NASA NSIDC Distributed Active Archive Center (DAAC), and the Exchange for Local Observations and Knowledge of the Arctic (ELOKA). If you have a question that is not answered here, please contact NSIDC User Services.

 

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Dig Tsho glacial lake in Nepal
A glacial lake is a body of water that originates from a glacier. It typically forms at the foot of a glacier, but may form on, in, or under it. As Earth’s climate warms, the world’s glaciers are shrinking, increasing freshwater outputs to all kinds of glacial lakes.
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On the landmasses surrounding the Arctic Ocean, tundra typically thrives. Tundra landscapes consist of low-profile, cold-adapted plants that eke out their tiny lives in short, cool summers. Since the early 1980s, though, satellites and ground-based
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A tipping point is a critical threshold where an incremental change could push a system over the edge to a new state. Two types of tipping points exist. One involves a rapid transition, like what happens when a canoe rocks back and forth. Eventually
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Climate models, also known as general circulation models or GCMs, use computers to simulate Earth’s climate. Scientists use climate models to predict weather, but unlike weather forecasts, the timespan is over decades or centuries rather than hours