Article
Article
- Earth Science
- Oceanography
- Arctic sea-ice monitoring
DISCLAIMER: This article is being kept online for historical purposes. Though accurate at last review, it is no longer being updated. The page may contain broken links or outdated information.
Arctic sea-ice monitoring
Article By:
Nghiem, Son V. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California.
Neumann, Gregory Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California.
Last reviewed:2007
DOI:https://doi.org/10.1036/1097-8542.YB071580
- Satellite scatterometer
- Minimal extent of summer sea ice
- Reduction of perennial sea ice
- Sea-ice melting process
- Implications of diminished sea ice
- Related Primary Literature
- Additional Reading
Arctic sea ice has undergone drastic change in recent years, emphasizing the critical role of satellite remote sensing to monitor Arctic change with a frequent coverage over large regions. Optical and multispectral sensors require clear sky and sufficient solar lighting. Microwave radiometers measure ice concentration, the fraction of ice-covered area over the total area, but cannot accurately detect different sea-ice classes. The satellite scatterometer, defined as a stable and accurate radar, is emerging as a versatile sensor for Earth observations and providing new capabilities for sea-ice classification and melt detection regardless of cloud cover and darkness.
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