SMOS sea ice product: Operational application and validation in the Barents Sea marginal ice zone
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- 作者：Lars Kaleschkea ; lars.kaleschke@uni-hamburg.de" class="auth_mail" title="E-mail the corresponding author ; Xiangshan Tian-Kunzea ; Nina Maaß ; a ; Alexander Beitscha ; b ; Andreas Werneckea ; Maciej Mierneckia ; Gerd Mü ; llerc ; Bjö ; rn H. Fockc ; d ; Andrea M.U. Gierischc ; e ; K. Heinke Schlü ; nzenc ; Thomas Pohlmanna ; Mikhail Dobrynina ; Stefan Hendricksf ; Jö ; lund Assengf ; Rü ; diger Gerdesf ; h ; Peter Jochmanng ; Nils Reimerg ; Jü ; rgen Holforti ; Christian Melsheimerj ; Georg Heygsterj ; Gunnar Spreenk ; j ; Sebastian Gerlandk ; Jennifer Kingk ; Niels Skoul ; Sten Schmidl Sø ; bjæ ; rgl ; Christian Haasm ; Friedrich Richtern ; Tâ ; nia Casaln
- 关键词：Soil moisture and ocean salinity (SMOS) mission ; L-Band radiometry ; Arctic ; Sea ice ; Sea ice thickness ; Retrieval model validation ; Airborne laser scanner ; Electromagnetic induction ; Sea ice forecast ; Ship routing
- 刊名：Remote Sensing of Environment
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：180
- 期：Complete
- 页码：264-273
- 全文大小：2450 K
文摘
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SMOS L-Band brightness temperatures can be used to derive sea ice thickness.
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SMOS sea ice thickness has been used for the initialization of a forecast model.
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Sea ice thickness validation data has been obtained in the Barents Sea in March 2014.
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For thickness up to about 1.5 m airborne radiometer is correlated with independent data.
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Current SMOS algorithms underestimate the mean thickness of thick deformed ice.