Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet

<p>The ERA5 reanalysis, recently made available by the European Centre for Medium-Range Weather Forecasts (ECMWF), is a new reanalysis product at a high resolution replacing ERA-Interim and is considered to provide the best climate reanalysis over Greenland to date. However, so far little is k...

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Glavni autori: A. Delhasse, C. Kittel, C. Amory, S. Hofer, D. van As, R. S. Fausto, X. Fettweis
Format: Članak
Jezik:English
Izdano: Copernicus Publications 2020-03-01
Serija:The Cryosphere
Online pristup:https://www.the-cryosphere.net/14/957/2020/tc-14-957-2020.pdf
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author A. Delhasse
C. Kittel
C. Amory
S. Hofer
S. Hofer
D. van As
R. S. Fausto
X. Fettweis
author_facet A. Delhasse
C. Kittel
C. Amory
S. Hofer
S. Hofer
D. van As
R. S. Fausto
X. Fettweis
author_sort A. Delhasse
collection DOAJ
description <p>The ERA5 reanalysis, recently made available by the European Centre for Medium-Range Weather Forecasts (ECMWF), is a new reanalysis product at a high resolution replacing ERA-Interim and is considered to provide the best climate reanalysis over Greenland to date. However, so far little is known about the performance of ERA5 over the Greenland Ice Sheet (GrIS). In this study, we compare the near-surface climate from the new ERA5 reanalysis to ERA-Interim, the Arctic System Reanalysis (ASR) as well as to a state-of-the-art polar regional climate model (MAR). The results show (1) that ERA5 does not outperform ERA-Interim significantly when compared with near-surface climate observations over GrIS, but ASR better models the near-surface temperature than both ERA reanalyses. (2) Polar regional climate models (e.g., MAR) are still a useful tool to downscale the GrIS climate compared to ERA5, as in particular the near-surface temperature in summer has a key role for representing snow and ice processes such as the surface melt. However, assimilating satellite data and using a more recent radiative scheme enable both ERA and ASR reanalyses to represent more satisfactorily than MAR the downward solar and infrared fluxes. (3) MAR near-surface climate is not affected when forced at its lateral boundaries by either ERA5 or ERA-Interim. Therefore, forcing polar regional climate models with ERA5 starting from 1950 will enable long and homogeneous surface mass balance reconstructions.</p>
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spelling doaj.art-bcc573040f944d7199fe6acd0871b5d02022-12-22T01:08:10ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242020-03-011495796510.5194/tc-14-957-2020Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice SheetA. Delhasse0C. Kittel1C. Amory2S. Hofer3S. Hofer4D. van As5R. S. Fausto6X. Fettweis7Laboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, BelgiumLaboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, BelgiumLaboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, BelgiumLaboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, BelgiumSchool of Geographical Sciences, University of Bristol, Bristol, UKGeological Survey of Denmark and Greenland (GEUS), 1350 Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), 1350 Copenhagen, DenmarkLaboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, Belgium<p>The ERA5 reanalysis, recently made available by the European Centre for Medium-Range Weather Forecasts (ECMWF), is a new reanalysis product at a high resolution replacing ERA-Interim and is considered to provide the best climate reanalysis over Greenland to date. However, so far little is known about the performance of ERA5 over the Greenland Ice Sheet (GrIS). In this study, we compare the near-surface climate from the new ERA5 reanalysis to ERA-Interim, the Arctic System Reanalysis (ASR) as well as to a state-of-the-art polar regional climate model (MAR). The results show (1) that ERA5 does not outperform ERA-Interim significantly when compared with near-surface climate observations over GrIS, but ASR better models the near-surface temperature than both ERA reanalyses. (2) Polar regional climate models (e.g., MAR) are still a useful tool to downscale the GrIS climate compared to ERA5, as in particular the near-surface temperature in summer has a key role for representing snow and ice processes such as the surface melt. However, assimilating satellite data and using a more recent radiative scheme enable both ERA and ASR reanalyses to represent more satisfactorily than MAR the downward solar and infrared fluxes. (3) MAR near-surface climate is not affected when forced at its lateral boundaries by either ERA5 or ERA-Interim. Therefore, forcing polar regional climate models with ERA5 starting from 1950 will enable long and homogeneous surface mass balance reconstructions.</p>https://www.the-cryosphere.net/14/957/2020/tc-14-957-2020.pdf
spellingShingle A. Delhasse
C. Kittel
C. Amory
S. Hofer
S. Hofer
D. van As
R. S. Fausto
X. Fettweis
Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
The Cryosphere
title Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
title_full Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
title_fullStr Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
title_full_unstemmed Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
title_short Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet
title_sort brief communication evaluation of the near surface climate in era5 over the greenland ice sheet
url https://www.the-cryosphere.net/14/957/2020/tc-14-957-2020.pdf
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