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Brief communication: Conventional assumptions involving the speed of radar waves in snow introduce systematic underestimates to sea ice thickness and seasonal growth rate estimates

Research output: Contribution to journalArticle

Original languageEnglish
Pages (from-to)251-260
Number of pages10
JournalCryosphere
Volume14
Issue number1
DOIs
DateAccepted/In press - 12 Dec 2019
DatePublished (current) - 27 Jan 2020

Abstract

Pan-Arctic sea ice thickness has been monitored over recent decades by satellite radar altimeters such as CryoSat-2, which emits Ku-band radar waves that are assumed in publicly available sea ice thickness products to penetrate overlying snow and scatter from the ice-snow interface. Here we examine two expressions for the time delay caused by slower radar wave propagation through the snow layer and related assumptions concerning the time evolution of overlying snow density. Two conventional treatments introduce systematic underestimates of up to 15 cm into ice thickness estimates and up to 10 cm into thermodynamic growth rate estimates over multi-year ice in winter. Correcting these biases would impact a wide variety of model projections, calibrations, validations and reanalyses.

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    Rights statement: This is the final published version of the article (version of record). It first appeared online via European Geosciences Union at https://doi.org/10.5194/tc-14-251-2020 . Please refer to any applicable terms of use of the publisher.

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    Licence: CC BY

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