Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim

We compare the main atmospheric drivers of the melt season over the Greenland Ice Sheet (GrIS) in ERA5 and ERA-Interim (ERAI) in their overlapping period 1979–2018. In summer, ERA5 differs significantly from ERAI, especially in the melt regions. Small-scale ERA5 − ERAI differences near the ice sheet...

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Main Authors: Krebs-Kanzow, Uta, Rodehacke, Christian B., Lohmann, Gerrit
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-525
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-525/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere110284 2024-01-07T09:43:34+01:00 Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim Krebs-Kanzow, Uta Rodehacke, Christian B. Lohmann, Gerrit 2023-12-06 application/pdf https://doi.org/10.5194/egusphere-2023-525 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-525/ eng eng doi:10.5194/egusphere-2023-525 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-525/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-525 2023-12-11T17:24:19Z We compare the main atmospheric drivers of the melt season over the Greenland Ice Sheet (GrIS) in ERA5 and ERA-Interim (ERAI) in their overlapping period 1979–2018. In summer, ERA5 differs significantly from ERAI, especially in the melt regions. Small-scale ERA5 − ERAI differences near the ice sheet's margins and over steep slopes can be explained by the different resolution, while the large-scale differences indicate a different representation of physical processes in the two reanalyses: averaged over the lower parts of the GrIS, the mean near-surface air temperature is 1 K lower, while the mean downward shortwave radiation at the surface is on average 15 W m −2 higher than in ERAI. Comparison with observational weather station data shows a significant warm bias in ERAI and, for ERA5, a significant positive bias in downward shortwave radiation. Consequently, methods that previously estimated the GrIS surface mass balance from the ERAI surface energy balance need to be carefully recalibrated before converting to ERA5 forcing. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We compare the main atmospheric drivers of the melt season over the Greenland Ice Sheet (GrIS) in ERA5 and ERA-Interim (ERAI) in their overlapping period 1979–2018. In summer, ERA5 differs significantly from ERAI, especially in the melt regions. Small-scale ERA5 − ERAI differences near the ice sheet's margins and over steep slopes can be explained by the different resolution, while the large-scale differences indicate a different representation of physical processes in the two reanalyses: averaged over the lower parts of the GrIS, the mean near-surface air temperature is 1 K lower, while the mean downward shortwave radiation at the surface is on average 15 W m −2 higher than in ERAI. Comparison with observational weather station data shows a significant warm bias in ERAI and, for ERA5, a significant positive bias in downward shortwave radiation. Consequently, methods that previously estimated the GrIS surface mass balance from the ERAI surface energy balance need to be carefully recalibrated before converting to ERA5 forcing.
format Text
author Krebs-Kanzow, Uta
Rodehacke, Christian B.
Lohmann, Gerrit
spellingShingle Krebs-Kanzow, Uta
Rodehacke, Christian B.
Lohmann, Gerrit
Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
author_facet Krebs-Kanzow, Uta
Rodehacke, Christian B.
Lohmann, Gerrit
author_sort Krebs-Kanzow, Uta
title Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
title_short Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
title_full Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
title_fullStr Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
title_full_unstemmed Brief communication: Surface energy balance differences over Greenland between ERA5 and ERA-Interim
title_sort brief communication: surface energy balance differences over greenland between era5 and era-interim
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-525
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-525/
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-525
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-525/
op_doi https://doi.org/10.5194/egusphere-2023-525
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