An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature

The European Center for Medium-Range Weather Forecasts (ECMWF) released its latest reanalysis dataset named ERA5 in 2017. To assess the performance of ERA5 in Antarctica, we compare the near-surface temperature data from ERA5 and ERA-Interim with the measured data from 41 weather stations. ERA5 has...

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Published in:Atmosphere
Main Authors: Jiangping Zhu, Aihong Xie, Xiang Qin, Yetang Wang, Bing Xu, Yicheng Wang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12020217
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/2/217/ 2023-08-20T04:01:03+02:00 An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature Jiangping Zhu Aihong Xie Xiang Qin Yetang Wang Bing Xu Yicheng Wang agris 2021-02-05 application/pdf https://doi.org/10.3390/atmos12020217 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos12020217 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 2; Pages: 217 ERA5 ERA-Interim Antarctica air temperature in situ observations Text 2021 ftmdpi https://doi.org/10.3390/atmos12020217 2023-08-01T01:01:01Z The European Center for Medium-Range Weather Forecasts (ECMWF) released its latest reanalysis dataset named ERA5 in 2017. To assess the performance of ERA5 in Antarctica, we compare the near-surface temperature data from ERA5 and ERA-Interim with the measured data from 41 weather stations. ERA5 has a strong linear relationship with monthly observations, and the statistical significant correlation coefficients (p < 0.05) are higher than 0.95 at all stations selected. The performance of ERA5 shows regional differences, and the correlations are high in West Antarctica and low in East Antarctica. Compared with ERA5, ERA-Interim has a slightly higher linear relationship with observations in the Antarctic Peninsula. ERA5 agrees well with the temperature observations in austral spring, with significant correlation coefficients higher than 0.90 and bias lower than 0.70 °C. The temperature trend from ERA5 is consistent with that from observations, in which a cooling trend dominates East Antarctica and West Antarctica, while a warming trend exists in the Antarctic Peninsula except during austral summer. Generally, ERA5 can effectively represent the temperature changes in Antarctica and its three subregions. Although ERA5 has bias, ERA5 can play an important role as a powerful tool to explore the climate change in Antarctica with sparse in situ observations. Text Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica West Antarctica MDPI Open Access Publishing Antarctic Antarctic Peninsula Austral East Antarctica The Antarctic West Antarctica Atmosphere 12 2 217
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ERA5
ERA-Interim
Antarctica
air temperature
in situ observations
spellingShingle ERA5
ERA-Interim
Antarctica
air temperature
in situ observations
Jiangping Zhu
Aihong Xie
Xiang Qin
Yetang Wang
Bing Xu
Yicheng Wang
An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
topic_facet ERA5
ERA-Interim
Antarctica
air temperature
in situ observations
description The European Center for Medium-Range Weather Forecasts (ECMWF) released its latest reanalysis dataset named ERA5 in 2017. To assess the performance of ERA5 in Antarctica, we compare the near-surface temperature data from ERA5 and ERA-Interim with the measured data from 41 weather stations. ERA5 has a strong linear relationship with monthly observations, and the statistical significant correlation coefficients (p < 0.05) are higher than 0.95 at all stations selected. The performance of ERA5 shows regional differences, and the correlations are high in West Antarctica and low in East Antarctica. Compared with ERA5, ERA-Interim has a slightly higher linear relationship with observations in the Antarctic Peninsula. ERA5 agrees well with the temperature observations in austral spring, with significant correlation coefficients higher than 0.90 and bias lower than 0.70 °C. The temperature trend from ERA5 is consistent with that from observations, in which a cooling trend dominates East Antarctica and West Antarctica, while a warming trend exists in the Antarctic Peninsula except during austral summer. Generally, ERA5 can effectively represent the temperature changes in Antarctica and its three subregions. Although ERA5 has bias, ERA5 can play an important role as a powerful tool to explore the climate change in Antarctica with sparse in situ observations.
format Text
author Jiangping Zhu
Aihong Xie
Xiang Qin
Yetang Wang
Bing Xu
Yicheng Wang
author_facet Jiangping Zhu
Aihong Xie
Xiang Qin
Yetang Wang
Bing Xu
Yicheng Wang
author_sort Jiangping Zhu
title An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
title_short An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
title_full An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
title_fullStr An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
title_full_unstemmed An Assessment of ERA5 Reanalysis for Antarctic Near-Surface Air Temperature
title_sort assessment of era5 reanalysis for antarctic near-surface air temperature
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12020217
op_coverage agris
geographic Antarctic
Antarctic Peninsula
Austral
East Antarctica
The Antarctic
West Antarctica
geographic_facet Antarctic
Antarctic Peninsula
Austral
East Antarctica
The Antarctic
West Antarctica
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
West Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
West Antarctica
op_source Atmosphere; Volume 12; Issue 2; Pages: 217
op_relation Climatology
https://dx.doi.org/10.3390/atmos12020217
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12020217
container_title Atmosphere
container_volume 12
container_issue 2
container_start_page 217
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