Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval

<p>In this study, we compare eight recently developed snow depth products over Arctic sea ice, which use satellite observations, modeling, or a combination of satellite and modeling approaches. These products are further compared against various ground-truth observations, including those from...

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Main Authors: L. Zhou, J. Stroeve, S. Xu, A. Petty, R. Tilling, M. Winstrup, P. Rostosky, I. R. Lawrence, G. E. Liston, A. Ridout, M. Tsamados, V. Nandan
Format: Article
Language:English
Published: Copernicus Publications 2021-01-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/15/345/2021/tc-15-345-2021.pdf
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author L. Zhou
J. Stroeve
J. Stroeve
J. Stroeve
S. Xu
S. Xu
A. Petty
A. Petty
R. Tilling
R. Tilling
M. Winstrup
M. Winstrup
P. Rostosky
I. R. Lawrence
G. E. Liston
A. Ridout
M. Tsamados
V. Nandan
author_facet L. Zhou
J. Stroeve
J. Stroeve
J. Stroeve
S. Xu
S. Xu
A. Petty
A. Petty
R. Tilling
R. Tilling
M. Winstrup
M. Winstrup
P. Rostosky
I. R. Lawrence
G. E. Liston
A. Ridout
M. Tsamados
V. Nandan
author_sort L. Zhou
collection DOAJ
description <p>In this study, we compare eight recently developed snow depth products over Arctic sea ice, which use satellite observations, modeling, or a combination of satellite and modeling approaches. These products are further compared against various ground-truth observations, including those from ice mass balance observations and airborne measurements. Large mean snow depth discrepancies are observed over the Atlantic and Canadian Arctic sectors. The differences between climatology and the snow products early in winter could be in part a result of the delaying in Arctic ice formation that reduces early snow accumulation, leading to shallower snowpacks at the start of the freeze-up season. These differences persist through spring despite overall more winter snow accumulation in the reanalysis-based products than in the climatologies. Among the products evaluated, the University of Washington (UW) snow depth product produces the deepest spring (March–April) snowpacks, while the snow product from the Danish Meteorological Institute (DMI) provides the shallowest spring snow depths. Most snow products show significant correlation with snow depths retrieved from Operational IceBridge (OIB) while correlations are quite low against buoy measurements, with no correlation and very low variability from University of Bremen and DMI products. Inconsistencies in reconstructed snow depth among the products, as well as differences between these products and in situ and airborne observations, can be partially attributed to differences in effective footprint and spatial–temporal coverage, as well as insufficient observations for validation/bias adjustments. Our results highlight the need for more targeted Arctic surveys over different spatial and temporal scales to allow for a more systematic comparison and fusion of airborne, in situ and remote sensing observations.</p>
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spelling doaj.art-35fc6c568293404589b534a1bb366bb92022-12-21T19:57:26ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242021-01-011534536710.5194/tc-15-345-2021Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrievalL. Zhou0J. Stroeve1J. Stroeve2J. Stroeve3S. Xu4S. Xu5A. Petty6A. Petty7R. Tilling8R. Tilling9M. Winstrup10M. Winstrup11P. Rostosky12I. R. Lawrence13G. E. Liston14A. Ridout15M. Tsamados16V. Nandan17Ministry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science, Tsinghua University, Beijing, ChinaCentre for Polar Observation and Modelling, Earth Sciences, University College London, London, UKCentre for Earth Observation Science, University of Manitoba, Winnipeg, CanadaNational Snow and Ice Data Center, University of Colorado, Boulder, CO, USAMinistry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science, Tsinghua University, Beijing, ChinaUniversity Corporation for Polar Research, Beijing, ChinaNASA Goddard Space Flight Center, Greenbelt, MD, USAEarth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USANASA Goddard Space Flight Center, Greenbelt, MD, USAEarth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USADTU Space, Technical University of Denmark, Lyngby, DenmarkDanish Meteorological Institute (DMI), Copenhagen, DenmarkInstitute of Environmental Physics, University of Bremen, Bremen, GermanyCentre for Polar Observation and Modelling, University of Leeds, Leeds, UKColorado State University, Cooperative Institute for Research in the Atmosphere (CIRA), Fort Collins, CO, USACentre for Polar Observation and Modelling, Earth Sciences, University College London, London, UKCentre for Polar Observation and Modelling, Earth Sciences, University College London, London, UKCentre for Earth Observation Science, University of Manitoba, Winnipeg, Canada<p>In this study, we compare eight recently developed snow depth products over Arctic sea ice, which use satellite observations, modeling, or a combination of satellite and modeling approaches. These products are further compared against various ground-truth observations, including those from ice mass balance observations and airborne measurements. Large mean snow depth discrepancies are observed over the Atlantic and Canadian Arctic sectors. The differences between climatology and the snow products early in winter could be in part a result of the delaying in Arctic ice formation that reduces early snow accumulation, leading to shallower snowpacks at the start of the freeze-up season. These differences persist through spring despite overall more winter snow accumulation in the reanalysis-based products than in the climatologies. Among the products evaluated, the University of Washington (UW) snow depth product produces the deepest spring (March–April) snowpacks, while the snow product from the Danish Meteorological Institute (DMI) provides the shallowest spring snow depths. Most snow products show significant correlation with snow depths retrieved from Operational IceBridge (OIB) while correlations are quite low against buoy measurements, with no correlation and very low variability from University of Bremen and DMI products. Inconsistencies in reconstructed snow depth among the products, as well as differences between these products and in situ and airborne observations, can be partially attributed to differences in effective footprint and spatial–temporal coverage, as well as insufficient observations for validation/bias adjustments. Our results highlight the need for more targeted Arctic surveys over different spatial and temporal scales to allow for a more systematic comparison and fusion of airborne, in situ and remote sensing observations.</p>https://tc.copernicus.org/articles/15/345/2021/tc-15-345-2021.pdf
spellingShingle L. Zhou
J. Stroeve
J. Stroeve
J. Stroeve
S. Xu
S. Xu
A. Petty
A. Petty
R. Tilling
R. Tilling
M. Winstrup
M. Winstrup
P. Rostosky
I. R. Lawrence
G. E. Liston
A. Ridout
M. Tsamados
V. Nandan
Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
The Cryosphere
title Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
title_full Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
title_fullStr Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
title_full_unstemmed Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
title_short Inter-comparison of snow depth over Arctic sea ice from reanalysis reconstructions and satellite retrieval
title_sort inter comparison of snow depth over arctic sea ice from reanalysis reconstructions and satellite retrieval
url https://tc.copernicus.org/articles/15/345/2021/tc-15-345-2021.pdf
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