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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

<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 exami...

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Principais autores: R. D. C. Mallett, I. R. Lawrence, J. C. Stroeve, J. C. Landy, M. Tsamados
Format: Artigo
Jezik:Inglês
Izdano: Copernicus Publications 2020-01-01
Serija:The Cryosphere
Online dostop:https://www.the-cryosphere.net/14/251/2020/tc-14-251-2020.pdf
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