A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies

Climate reanalyses provide key information to calibrate proxy records in regions with scarce direct observations. The climate reanalysis used to perform a proxy calibration should accurately reproduce the local climate variability. Here we present a regional scale evaluation of meteorological parame...

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Published in:Geosciences
Main Authors: Dieter Tetzner, Elizabeth Thomas, Claire Allen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/geosciences9070289
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spelling ftmdpi:oai:mdpi.com:/2076-3263/9/7/289/ 2023-08-20T04:01:11+02:00 A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies Dieter Tetzner Elizabeth Thomas Claire Allen agris 2019-06-29 application/pdf https://doi.org/10.3390/geosciences9070289 EN eng Multidisciplinary Digital Publishing Institute Geophysics https://dx.doi.org/10.3390/geosciences9070289 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 9; Issue 7; Pages: 289 climate reanalysis ERA5 ERA-Interim Antarctic Peninsula ice cores Antarctica winds Text 2019 ftmdpi https://doi.org/10.3390/geosciences9070289 2023-07-31T22:23:55Z Climate reanalyses provide key information to calibrate proxy records in regions with scarce direct observations. The climate reanalysis used to perform a proxy calibration should accurately reproduce the local climate variability. Here we present a regional scale evaluation of meteorological parameters using ERA-Interim and ERA5 reanalyses compared to in-situ observations from 13 automatic weather stations (AWS), located in the southern Antarctic Peninsula and Ellsworth Land, Antarctica. Both reanalyses seem to perform better in the escarpment area (>1000 m a.s.l) than on the coast. A significant improvement is observed in the performance of ERA5 over ERA-Interim. ERA5 is highly accurate, representing the magnitude and variability of near-surface air temperature and wind regimes. The higher spatial and temporal resolution provided by ERA5 reduces significantly the cold coastal biases identified in ERA-Interim and increases the accuracy representing the wind direction and wind speed in the escarpment. The slight underestimation in the wind speed obtained from the reanalyses could be attributed to an interplay of topographic factors and the effect of local wind regimes. Three sites in this region are highlighted for their potential for ice core studies. These sites are likely to provide accurate proxy calibrations for future palaeoclimatic reconstructions. Text Antarc* Antarctic Antarctic Peninsula Antarctica ice core MDPI Open Access Publishing Antarctic Antarctic Peninsula Ellsworth Land ENVELOPE(-85.000,-85.000,-75.000,-75.000) Geosciences 9 7 289
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic climate reanalysis
ERA5
ERA-Interim
Antarctic Peninsula
ice cores
Antarctica
winds
spellingShingle climate reanalysis
ERA5
ERA-Interim
Antarctic Peninsula
ice cores
Antarctica
winds
Dieter Tetzner
Elizabeth Thomas
Claire Allen
A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
topic_facet climate reanalysis
ERA5
ERA-Interim
Antarctic Peninsula
ice cores
Antarctica
winds
description Climate reanalyses provide key information to calibrate proxy records in regions with scarce direct observations. The climate reanalysis used to perform a proxy calibration should accurately reproduce the local climate variability. Here we present a regional scale evaluation of meteorological parameters using ERA-Interim and ERA5 reanalyses compared to in-situ observations from 13 automatic weather stations (AWS), located in the southern Antarctic Peninsula and Ellsworth Land, Antarctica. Both reanalyses seem to perform better in the escarpment area (>1000 m a.s.l) than on the coast. A significant improvement is observed in the performance of ERA5 over ERA-Interim. ERA5 is highly accurate, representing the magnitude and variability of near-surface air temperature and wind regimes. The higher spatial and temporal resolution provided by ERA5 reduces significantly the cold coastal biases identified in ERA-Interim and increases the accuracy representing the wind direction and wind speed in the escarpment. The slight underestimation in the wind speed obtained from the reanalyses could be attributed to an interplay of topographic factors and the effect of local wind regimes. Three sites in this region are highlighted for their potential for ice core studies. These sites are likely to provide accurate proxy calibrations for future palaeoclimatic reconstructions.
format Text
author Dieter Tetzner
Elizabeth Thomas
Claire Allen
author_facet Dieter Tetzner
Elizabeth Thomas
Claire Allen
author_sort Dieter Tetzner
title A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
title_short A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
title_full A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
title_fullStr A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
title_full_unstemmed A Validation of ERA5 Reanalysis Data in the Southern Antarctic Peninsula—Ellsworth Land Region, and Its Implications for Ice Core Studies
title_sort validation of era5 reanalysis data in the southern antarctic peninsula—ellsworth land region, and its implications for ice core studies
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/geosciences9070289
op_coverage agris
long_lat ENVELOPE(-85.000,-85.000,-75.000,-75.000)
geographic Antarctic
Antarctic Peninsula
Ellsworth Land
geographic_facet Antarctic
Antarctic Peninsula
Ellsworth Land
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
ice core
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
ice core
op_source Geosciences; Volume 9; Issue 7; Pages: 289
op_relation Geophysics
https://dx.doi.org/10.3390/geosciences9070289
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences9070289
container_title Geosciences
container_volume 9
container_issue 7
container_start_page 289
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