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Differences Between ICESat and CryoSat-2 Sea Ice Thicknesses Over the Arctic: Consequences for Analyzing the Ice Volume Trend

Cited 5 time in Web of Science Cited 7 time in Scopus
Authors

Kim, Jong-Min; Sohn, Byung-Ju; Lee, Sang-Moo; Tonboe, Rasmus Tage; Kang, Eui-Jong; Kim, Hyun-Cheol

Issue Date
2020-11
Publisher
American Geophysical Union
Citation
Journal of geophysical research - Atmospheres, Vol.125 No.22, p. e2020JD033103
Abstract
Two sources of readily available and non-overlapping space-borne data on sea ice thickness over the Arctic (i.e., Ice, Cloud, and land Elevation Satellite [ICESat] and CryoSat-2 [CS2]) were compared using overlapping thermal microwave radiometer data to examine their respective differences. As a bridge connecting these two data sets, data on the vertically polarized emissivity difference between 10.65 and 18.7 GHz derived from the Advanced Microwave Sounding Radiometer were related to ICESat and CS2 thickness values via regression. The results indicate that there are substantial and systematic differences in the ice thickness between these two data sets over the Arctic; ICESat ice thickness was systematically lower than that of CS2 by similar to 50 cm, compared to ice thickness from Operation IceBridge and upper looking sonar data. The CS2 thickness observed later than that of ICESat was found to be thicker, contradicting the thinning expected under global warming conditions. Correcting for the 50-cm difference between ICESat or CS2 data revealed trends in ice volume that are consistent with the expected and modeled declines in the Pan-Arctic Ice-Ocean Modeling and Assimilation System data, further corroborating the 50 cm of relative bias observed between the two data sets.
ISSN
2169-897X
URI
https://hdl.handle.net/10371/201047
DOI
https://doi.org/10.1029/2020JD033103
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  • College of Natural Sciences
  • Department of Earth and Environmental Sciences
Research Area Data Assimilation for Numerical Weather Prediction, Radiative Transfer Modeling, Satellite Remote Sensing

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