The ERA5-Land soil temperature bias in permafrost regions
ERA5-Land (ERA5L) is a reanalysis product derived by running the land component of ERA5 at increased resolution. This study evaluates ERA5L soil temperature in permafrost regions based on observations and published permafrost products. We find that ERA5L overestimates soil temperature in northern Ca...
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Online Access: | https://ir.library.carleton.ca/pub/27959 https://doi.org/10.5194/tc-14-2581-2020 |
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ftcarletonunivir:oai:carleton.ca:27959 2023-05-15T13:02:57+02:00 The ERA5-Land soil temperature bias in permafrost regions Cao, B. (Bin) Gruber, S. (Stephan) Zheng, D. (Donghai) Li, X. (Xin) 2020-08-12 application/pdf https://ir.library.carleton.ca/pub/27959 https://doi.org/10.5194/tc-14-2581-2020 en eng https://ir.library.carleton.ca/pub/27959 doi:10.5194/tc-14-2581-2020 info:eu-repo/semantics/openAccess Cryosphere vol. 14 no. 8, pp. 2581-2595 info:eu-repo/semantics/article 2020 ftcarletonunivir https://doi.org/10.5194/tc-14-2581-2020 2022-02-06T21:47:41Z ERA5-Land (ERA5L) is a reanalysis product derived by running the land component of ERA5 at increased resolution. This study evaluates ERA5L soil temperature in permafrost regions based on observations and published permafrost products. We find that ERA5L overestimates soil temperature in northern Canada and Alaska but underestimates it in mid-low latitudes, leading to an average bias of -0.08 ĝ C. The warm bias of ERA5L soil is stronger in winter than in other seasons. As calculated from its soil temperature, ERA5L overestimates active-layer thickness and underestimates near-surface ( <1.89< Article in Journal/Newspaper Active layer thickness permafrost Alaska Carleton University's Institutional Repository Canada The Cryosphere 14 8 2581 2595 |
institution |
Open Polar |
collection |
Carleton University's Institutional Repository |
op_collection_id |
ftcarletonunivir |
language |
English |
description |
ERA5-Land (ERA5L) is a reanalysis product derived by running the land component of ERA5 at increased resolution. This study evaluates ERA5L soil temperature in permafrost regions based on observations and published permafrost products. We find that ERA5L overestimates soil temperature in northern Canada and Alaska but underestimates it in mid-low latitudes, leading to an average bias of -0.08 ĝ C. The warm bias of ERA5L soil is stronger in winter than in other seasons. As calculated from its soil temperature, ERA5L overestimates active-layer thickness and underestimates near-surface ( <1.89< |
format |
Article in Journal/Newspaper |
author |
Cao, B. (Bin) Gruber, S. (Stephan) Zheng, D. (Donghai) Li, X. (Xin) |
spellingShingle |
Cao, B. (Bin) Gruber, S. (Stephan) Zheng, D. (Donghai) Li, X. (Xin) The ERA5-Land soil temperature bias in permafrost regions |
author_facet |
Cao, B. (Bin) Gruber, S. (Stephan) Zheng, D. (Donghai) Li, X. (Xin) |
author_sort |
Cao, B. (Bin) |
title |
The ERA5-Land soil temperature bias in permafrost regions |
title_short |
The ERA5-Land soil temperature bias in permafrost regions |
title_full |
The ERA5-Land soil temperature bias in permafrost regions |
title_fullStr |
The ERA5-Land soil temperature bias in permafrost regions |
title_full_unstemmed |
The ERA5-Land soil temperature bias in permafrost regions |
title_sort |
era5-land soil temperature bias in permafrost regions |
publishDate |
2020 |
url |
https://ir.library.carleton.ca/pub/27959 https://doi.org/10.5194/tc-14-2581-2020 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Active layer thickness permafrost Alaska |
genre_facet |
Active layer thickness permafrost Alaska |
op_source |
Cryosphere vol. 14 no. 8, pp. 2581-2595 |
op_relation |
https://ir.library.carleton.ca/pub/27959 doi:10.5194/tc-14-2581-2020 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-14-2581-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
8 |
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2581 |
op_container_end_page |
2595 |
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1766324913949376512 |