Combined SMOS and SMAP sea ice thickness Arctic

• Main Authors: Schmitt, Amelie, Kaleschke, Lars
• Format: Dataset
• Language: unknown
• Published: Zenodo 2018
• Subjects: Sea ice; Sea ice thickness; SMOS; SMAP; L-band; Arctic; Polar
• Online Access: https://dx.doi.org/10.5281/zenodo.1631856; https://zenodo.org/record/1631856

This data set contains Arctic sea ice thicknesses derived from L-band passive microwave brightness temperatures. For this purpose, brightness temperatures at 40° incidence angle from the SMOS (Soil Moisture and Ocean Salinity) and SMAP (Soil Moisture Active Passive) satellites were combined to a homogenised data set (see also related data sets). Sea ice thicknesses were then derived using the algorithm described in Tian-Kunze et al. (2014). Data are generally produced for the freeze-up period from 15 October to 15 April. This data set contains data from on 1 April 2015 (first available SMAP data) to 15 April 2015 and for the winter seasons 2015/16 to 2017/18. A detailed description of the data set can be found Schmitt and Kaleschke (2018) and in the document 1_Documentation_Combined_SIT.pdf . Please note : Sea ice thicknesses from L-band are most suitable for thin ice and reach saturation for thicker sea ice (above 0.5 m - 1 m, depending on ice salinity and temperature). Thickness values with a saturation ratio of 100 % should be discarded (depending on the application)! Version 1.0 of this data set is based on SMOS version v620 and SMAP version 3 data. The files contain the following data fields: sea_ice_thickness - sea ice thickness with post-processing to account for the thickness distribution plane_layer_thickness - sea ice thickness using the plane layer assumption thickness_uncertainty_upper - upper limit of the sea ice thickness uncertainty interval thickness_uncertainty_lower - lower limit of the sea ice thickness uncertainty interval saturation_ratio - ratio of plane layer thickness and maximum retrievable thickness (%) TB_intensity - brightness temperature intensity combined from SMOS and SMAP at 40° incidence angle The grid coordinates are provided as a separate file Latlon_e12.5.nc : {"references": ["Schmitt, A. U. and Kaleschke, L. (2018). A Consistent Combination of Brightness Temperatures from SMOS and SMAP over Polar Oceans for Sea Ice Applications. Remote Sensing, 10(4), 553. doi: https://doi.org/10.3390/rs10040553", "Tian-Kunze, X.; Kaleschke, L.; Maa\u00df, N.; M\u00e4kynen, M.; Serra, N.; Drusch, M.; Krumpen, T. SMOS-derived thin sea ice thickness: algorithm baseline, product specifications and initial verification. Cryosphere 2014, 8, 997\u20131018. doi: https://doi.org/10.5194/tc-8-997-2014"]}