Definitions
(Land)fast ice. Sea ice attached to the shore or near-shore sea bed.
Nunatak. A mountain peak protruding through glacier ice.
Introduction
Remote sensing of the cryosphere has a 50 year history. We begin with an historical overview of aerial photography of the cryosphere – mainly glaciers and ice caps – and then proceed to satellite imagery and data for each of the major components of the cryosphere. In turn, we consider glaciers, snow cover, freshwater ice, sea ice, ice sheets and ice shelves, icebergs, and frozen ground.
Aerial photography
Glaciers and ice caps
Remote sensing of the cryosphere began with both vertical and oblique aerial photography of glaciers and ice caps. A massive campaign to photograph the Canadian Arctic was undertaken in the late 1940s–1950s (Dunbar and Greenway, 1956) and the photography covered all land areas. The US Geological Survey (USGS) photographed numerous glaciers in western North America and Alaska beginning in the 1950s (Post, 2005: http://earthweb.ess.washington.edu/EPIC/Collections/Post/index.htm...
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© 2014 Springer Science+Business Media New York
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Barry, R. (2014). Cryosphere, Measurements and Applications. In: Njoku, E.G. (eds) Encyclopedia of Remote Sensing. Encyclopedia of Earth Sciences Series. Springer, New York, NY. https://doi.org/10.1007/978-0-387-36699-9_28
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DOI: https://doi.org/10.1007/978-0-387-36699-9_28
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Publisher Name: Springer, New York, NY
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