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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 3
The Cryosphere, 4, 373-380, 2010
https://doi.org/10.5194/tc-4-373-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 4, 373-380, 2010
https://doi.org/10.5194/tc-4-373-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Sep 2010

Research article | 20 Sep 2010

The relation between sea ice thickness and freeboard in the Arctic

V. Alexandrov2,1, S. Sandven2,3, J. Wahlin2, and O. M. Johannessen2 V. Alexandrov et al.
  • 1Nansen International Environmental and Remote Sensing Center (NIERSC), 14th Line of Vasilevsky Island, 7, office 49, 199034 St. Petersburg, Russia
  • 2Nansen Environmental and Remote Sensing Center (NERSC), Thormoehlensgate 47, 5006 Bergen, Norway
  • 3Department of Arctic Geophysics, University of Svalbard (UNIS), 9171 Longyearbyen, Norway

Abstract. Retrieval of Arctic sea ice thickness from CryoSat-2 radar altimeter freeboard data requires observational data to verify the relation between these two variables. In this study in-situ ice and snow data from 689 observation sites, obtained during the Sever expeditions in the 1980s, have been used to establish an empirical relation between thickness and freeboard of FY ice in late winter. Estimates of mean and variability of snow depth, snow density and ice density were produced on the basis of many field observations. These estimates have been used in the hydrostatic equilibrium equation to retrieve ice thickness as a function of ice freeboard, snow depth and snow/ice density. The accuracy of the ice thickness retrieval has been calculated from the estimated variability in ice and snow parameters and error of ice freeboard measurements. It is found that uncertainties of ice density and freeboard are the major sources of error in ice thickness calculation. For FY ice, retrieval of ≈ 1.0 m (2.0 m) thickness has an uncertainty of 46% (37%), and for MY ice, retrieval of 2.4 m (3.0 m) thickness has an uncertainty of 20% (18%), assuming that the freeboard error is ± 0.03 m for both ice types. For MY ice the main uncertainty is ice density error, since the freeboard error is relatively smaller than that for FY ice. If the freeboard error can be reduced to 0.01 m by averaging measurements from CryoSat-2, the error in thickness retrieval is reduced to about 32% for a 1.0 m thick FY floe and to about 18% for a 2.4 m thick MY floe. The remaining error is dominated by uncertainty in ice density. Provision of improved ice density data is therefore important for accurate retrieval of ice thickness from CryoSat-2 data.

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