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

<p>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...

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Bibliographic Details
Main Authors: R. D. C. Mallett, I. R. Lawrence, J. C. Stroeve, J. C. Landy, M. Tsamados
Format: Article
Language:English
Published: Copernicus Publications 2020-01-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/14/251/2020/tc-14-251-2020.pdf