Retrievals of Arctic Sea-Ice Volume and Its Trend Significantly Affected by Interannual Snow Variability
- Max Planck Inst. for Meteorology, Hamburg (Germany)
- Technical Univ. of Denmark, Lyngby (Denmark)
We estimate the uncertainty of satellite-retrieved Arctic sea-ice thickness, sea-ice volume, and their trends stemming from the lack of reliable snow-thickness observations. To illustrate, we simulate a Cryosat2-type ice-thickness retrieval in an ocean-model simulation forced by atmospheric reanalysis, pretending that only freeboard is known as model output. We then convert freeboard to sea-ice thickness using different snow climatologies and compare the resulting sea-ice thickness retrievals to each other and to the real sea-ice thickness of the reanalysis-forced simulation. We postulate that different snow climatologies cause significant differences in the obtained ice thickness and ice volume. Moreover, we show that Arctic ice-volume trends derived from ice-thickness retrievals using any snow-depth climatology are highly unreliable because the estimated trend in ice volume can strongly be influenced by the neglected interannual variability in snow volume.
- Research Organization:
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). National Energy Research Scientific Computing Center (NERSC)
- Sponsoring Organization:
- USDOE Office of Science (SC)
- OSTI ID:
- 1544162
- Journal Information:
- Geophysical Research Letters, Vol. 45, Issue 21; ISSN 0094-8276
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
Web of Science
Climate Models as Guidance for the Design of Observing Systems: the Case of Polar Climate and Sea Ice Prediction
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journal | November 2019 |
Retrieval of Snow Depth over Arctic Sea Ice Using a Deep Neural Network
|
journal | December 2019 |
Climate Models as Guidance for the Design of Observing Systems - The case of Polar Climate and Sea Ice Prediction | text | January 2020 |
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