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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: Cao, B. (Bin), Gruber, S. (Stephan), Zheng, D. (Donghai), Li, X. (Xin)
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://ir.library.carleton.ca/pub/27959
https://doi.org/10.5194/tc-14-2581-2020
id ftcarletonunivir:oai:carleton.ca:27959
record_format openpolar
spelling 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
container_start_page 2581
op_container_end_page 2595
_version_ 1766324913949376512