Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice

Abstract Satellite observations of sea ice freeboard are integral to the estimation of sea ice thickness. It is commonly assumed that radar pulses from satellite‐mounted Ku‐band altimeters penetrate through the snow and reflect from the snow‐ice interface. We would therefore expect a negative correl...

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Published in:Geophysical Research Letters
Main Authors: Carmen Nab, Robbie Mallett, William Gregory, Jack Landy, Isobel Lawrence, Rosemary Willatt, Julienne Stroeve, Michel Tsamados
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL100696
https://doaj.org/article/46001f2b02c34afdb2a24d7876aa3382
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spelling ftdoajarticles:oai:doaj.org/article:46001f2b02c34afdb2a24d7876aa3382 2024-09-15T18:34:33+00:00 Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice Carmen Nab Robbie Mallett William Gregory Jack Landy Isobel Lawrence Rosemary Willatt Julienne Stroeve Michel Tsamados 2023-01-01T00:00:00Z https://doi.org/10.1029/2022GL100696 https://doaj.org/article/46001f2b02c34afdb2a24d7876aa3382 EN eng Wiley https://doi.org/10.1029/2022GL100696 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL100696 https://doaj.org/article/46001f2b02c34afdb2a24d7876aa3382 Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023) Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL100696 2024-08-05T17:49:23Z Abstract Satellite observations of sea ice freeboard are integral to the estimation of sea ice thickness. It is commonly assumed that radar pulses from satellite‐mounted Ku‐band altimeters penetrate through the snow and reflect from the snow‐ice interface. We would therefore expect a negative correlation between snow accumulation and radar freeboard measurements, as increased snow loading weighs the ice floe down. In this study we produce daily resolution radar freeboard products from the CryoSat‐2 and Sentinel‐3 altimeters via a recently developed optimal interpolation scheme. We find statistically significant (p < 0.05) positive correlations between radar freeboard anomalies and modeled snow accumulation. This suggests that, in the period after snowfall, radar pulses are not scattering from the snow‐ice interface as commonly assumed. Our results offer satellite‐based evidence of winter Ku‐band radar scattering above the snow‐ice interface, violating a key assumption in sea ice thickness retrievals. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 2
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geophysics. Cosmic physics
QC801-809
spellingShingle Geophysics. Cosmic physics
QC801-809
Carmen Nab
Robbie Mallett
William Gregory
Jack Landy
Isobel Lawrence
Rosemary Willatt
Julienne Stroeve
Michel Tsamados
Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
topic_facet Geophysics. Cosmic physics
QC801-809
description Abstract Satellite observations of sea ice freeboard are integral to the estimation of sea ice thickness. It is commonly assumed that radar pulses from satellite‐mounted Ku‐band altimeters penetrate through the snow and reflect from the snow‐ice interface. We would therefore expect a negative correlation between snow accumulation and radar freeboard measurements, as increased snow loading weighs the ice floe down. In this study we produce daily resolution radar freeboard products from the CryoSat‐2 and Sentinel‐3 altimeters via a recently developed optimal interpolation scheme. We find statistically significant (p < 0.05) positive correlations between radar freeboard anomalies and modeled snow accumulation. This suggests that, in the period after snowfall, radar pulses are not scattering from the snow‐ice interface as commonly assumed. Our results offer satellite‐based evidence of winter Ku‐band radar scattering above the snow‐ice interface, violating a key assumption in sea ice thickness retrievals.
format Article in Journal/Newspaper
author Carmen Nab
Robbie Mallett
William Gregory
Jack Landy
Isobel Lawrence
Rosemary Willatt
Julienne Stroeve
Michel Tsamados
author_facet Carmen Nab
Robbie Mallett
William Gregory
Jack Landy
Isobel Lawrence
Rosemary Willatt
Julienne Stroeve
Michel Tsamados
author_sort Carmen Nab
title Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
title_short Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
title_full Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
title_fullStr Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
title_full_unstemmed Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice
title_sort synoptic variability in satellite altimeter‐derived radar freeboard of arctic sea ice
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL100696
https://doaj.org/article/46001f2b02c34afdb2a24d7876aa3382
genre Sea ice
genre_facet Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL100696
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL100696
https://doaj.org/article/46001f2b02c34afdb2a24d7876aa3382
op_doi https://doi.org/10.1029/2022GL100696
container_title Geophysical Research Letters
container_volume 50
container_issue 2
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