SMOS-derived thin sea ice thickness: algorithm baseline, product specifications and initial verification.

Tian-Kunze, Xiangshan, Kaleschke, Lars, Maaß, Nina, Mäkynen, Marko, Serra, N., Drusch, Matthias and Krumpen, Thomas (2014) SMOS-derived thin sea ice thickness: algorithm baseline, product specifications and initial verification. The Cryosphere, 8 (3). pp. 997-1018. DOI 10.5194/tc-8-997-2014.

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Supplementary data:


Following the launch of ESA's Soil Moisture and Ocean Salinity (SMOS) mission, it has been shown that brightness temperatures at a low microwave frequency of 1.4 GHz (L-band) are sensitive to sea ice properties. In the first demonstration study, sea ice thickness up to 50 cm has been derived using a semi-empirical algorithm with constant tie-points. Here, we introduce a novel iterative retrieval algorithm that is based on a thermodynamic sea ice model and a three-layer radiative transfer model, which explicitly takes variations of ice temperature and ice salinity into account. In addition, ice thickness variations within the SMOS spatial resolution are considered through a statistical thickness distribution function derived from high-resolution ice thickness measurements from NASA's Operation IceBridge campaign. This new algorithm has been used for the continuous operational production of a SMOS-based sea ice thickness data set from 2010 on. The data set is compared to and validated with estimates from assimilation systems, remote sensing data, and airborne electromagnetic sounding data. The comparisons show that the new retrieval algorithm has a considerably better agreement with the validation data and delivers a more realistic Arctic-wide ice thickness distribution than the algorithm used in the previous study (Kaleschke et al., 2012).

Document Type: Article
Keywords: Soil Moisture and Ocean Salinity, SMOS; Sea ice thickness; Retrieval algorithm
Refereed: Yes
Open Access Journal?: Yes
Publisher: Copernicus Publications (EGU)
Projects: Laptev Sea System, Transdrift
Date Deposited: 13 Mar 2015 13:17
Last Modified: 13 Mar 2015 13:17

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