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Title: Combined SMOS and SMAP sea ice thickness Arctic

Type Dataset Schmitt, Amelie, Kaleschke, Lars (2018): Combined SMOS and SMAP sea ice thickness Arctic. Zenodo. Dataset. https://zenodo.org/record/1631856

Authors: Schmitt, Amelie (University of Hamburg) ; Kaleschke, Lars (Max-Planck-Institute of Meteorology) ;

Links

Summary

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

More information

  • DOI: 10.5281/zenodo.1631856

Subjects

  • Sea ice, Sea ice thickness, SMOS, SMAP, L-band, Arctic, Polar

Dates

  • Publication date: 2018
  • Issued: November 28, 2018

Notes

Other: {"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"]}

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Funding Information

AwardnumberAwarduriFunderidentifierFunderidentifiertypeFundername
640161info:eu-repo/grantAgreement/EC/H2020/640161/10.13039/100010661Crossref Funder IDEuropean Commission

Format

electronic resource

Relateditems

DescriptionItem typeRelationshipUri
Citeshttps://doi.org/10.3390/rs10040553
Citeshttps://doi.org/10.5194/tc-8-997-2014
IsSupplementTohttps://doi.org/10.5281/zenodo.1631762
IsSupplementTohttps://doi.org/10.5281/zenodo.1627380
IsVersionOfhttps://doi.org/10.5281/zenodo.1631855
IsPartOfhttps://zenodo.org/communities/zenodo