Surface-Based Ku- and Ka-band Polarimetric Radar for Sea Ice Studies

To improve our understanding of how snow properties influence sea ice thickness retrievals from presently operational and upcoming satellite radar altimeter missions, as well as investigating the potential for combining dual frequencies to simultaneously map snow depth and sea ice thickness, a new,...

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Bibliographic Details
Main Authors: Stroeve, Julienne, Nandan, Vishnu, Willatt, Rosemary, Tonboe, Rasmus, Hendricks, Stefan, Ricker, Robert, Mead, James, Huntemann, Marcus, Itkin, Polona, Schneebeli, Martin, Krampe, Daniela, Spreen, Gunnar, Wilkinson, Jeremy, Matero, Ilkka, Hoppmann, Mario, Mallett, Robbie, Tsamados, Michel
Format: Text
Language:English
Published: 2020
Subjects:
Arctic
Sea ice
Online Access:https://doi.org/10.5194/tc-2020-151
https://tc.copernicus.org/preprints/tc-2020-151/
Description
Summary:To improve our understanding of how snow properties influence sea ice thickness retrievals from presently operational and upcoming satellite radar altimeter missions, as well as investigating the potential for combining dual frequencies to simultaneously map snow depth and sea ice thickness, a new, surface-based, fully-polarimetric Ku- and Ka-band radar (KuKa radar) was built and deployed during the 2019–2020 year-long MOSAiC International Arctic drift expedition. This instrument, built to operate both as an altimeter (stare mode) and a scatterometer (scanning mode), provided the first in situ Ku- and Ka-band dual frequency radar observations from autumn freeze-up through mid-winter, and covering newly formed ice in leads, first-year and second-year ice floes. Data gathered in the altimeter mode, will be used to investigate the potential for estimating snow depth as the difference between dominant radar scattering horizons in the Ka- and Ku-band data. In the scatterometer mode, the Ku- and Ka-band radars operated under a wide range of azimuth and incidence angle ranges, continuously assessing changes in the polarimetric radar backscatter and derived polarimetric parameters, as snow properties varied under varying atmospheric conditions. These observations allow for characterizing radar backscatter responses to changes in atmospheric and surface geophysical conditions. In this paper, we describe the KuKa radar and illustrate examples of these data and demonstrate their potential for these investigations.

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