Danish Meteorological Institute, Copenhagen, Denmark
Vishnu Nandan
Center for Earth Observation Sciences (CEOS), Clayton H. Riddell Faculty of Environment,
Earth, and Resources, University of Manitoba, Winnipeg, Canada
Cryosphere Climate Research Group, Department of Geography, University of Calgary, Calgary, Canada
John Yackel
Cryosphere Climate Research Group, Department of Geography, University of Calgary, Calgary, Canada
National Space Institute, Technical University of Denmark, Lyngby, Denmark
Julienne Stroeve
Center for Earth Observation Sciences (CEOS), Clayton H. Riddell Faculty of Environment,
Earth, and Resources, University of Manitoba, Winnipeg, Canada
Earth Sciences, University College London, London, UK
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Total article views: 2,121 (including HTML, PDF, and XML)
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A relationship between the Ku-band radar scattering horizon and snow depth is found using a radar scattering model. This relationship has implications for (1) the use of snow climatology in the conversion of satellite radar freeboard into sea ice thickness and (2) the impact of variability in measured snow depth on the derived ice thickness. For both 1 and 2, the impact of using a snow climatology versus the actual snow depth is relatively small.
A relationship between the Ku-band radar scattering horizon and snow depth is found using a...
