The Record-Breaking High Temperature over Europe in June of 2019

Observational and reanalysis data show that the surface air temperature (SAT) over most parts of Europe in June of 2019 broke the highest temperature on record. In this study, we investigate the factors for the formation of this record-breaking high temperature over Europe, focusing on the role of a...

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Published in:Atmosphere
Main Authors: Wei Zhao, Ningfang Zhou, Shangfeng Chen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11050524
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spelling ftmdpi:oai:mdpi.com:/2073-4433/11/5/524/ 2023-08-20T04:08:16+02:00 The Record-Breaking High Temperature over Europe in June of 2019 Wei Zhao Ningfang Zhou Shangfeng Chen agris 2020-05-20 application/pdf https://doi.org/10.3390/atmos11050524 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/atmos11050524 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 5; Pages: 524 Europe record-breaking high temperature atmospheric wave train Text 2020 ftmdpi https://doi.org/10.3390/atmos11050524 2023-07-31T23:31:25Z Observational and reanalysis data show that the surface air temperature (SAT) over most parts of Europe in June of 2019 broke the highest temperature on record. In this study, we investigate the factors for the formation of this record-breaking high temperature over Europe, focusing on the role of atmospheric circulation anomalies. A strong anomalous anticyclone appeared over Europe, with a quasi-barotropic vertical structure. On one hand, the downward motion anomalies associated with this anomalous anticyclone led to less cloud cover and an increase in downward shortwave radiation, which contributed to the SAT warming over Europe. On the other hand, southerly wind anomalies to the west side of the anomalous anticyclone also resulted in SAT warming via carrying warmer and wetter air northward from lower latitudes. The formation of the anticyclonic anomaly over Europe in June of 2019 was closely related to an atmospheric wave train propagating eastward from the mid-high latitudes of the North Atlantic to Eurasia. The atmospheric wave train over the North Atlantic–Eurasia region is suggested to be mainly related to the Atlantic–Eurasia teleconnection pattern. Further analysis indicates that a decrease in the local soil moisture over Europe may also have escalated the surface temperature warming through a positive land–atmosphere feedback. Text North Atlantic MDPI Open Access Publishing Atmosphere 11 5 524
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Europe
record-breaking high temperature
atmospheric wave train
spellingShingle Europe
record-breaking high temperature
atmospheric wave train
Wei Zhao
Ningfang Zhou
Shangfeng Chen
The Record-Breaking High Temperature over Europe in June of 2019
topic_facet Europe
record-breaking high temperature
atmospheric wave train
description Observational and reanalysis data show that the surface air temperature (SAT) over most parts of Europe in June of 2019 broke the highest temperature on record. In this study, we investigate the factors for the formation of this record-breaking high temperature over Europe, focusing on the role of atmospheric circulation anomalies. A strong anomalous anticyclone appeared over Europe, with a quasi-barotropic vertical structure. On one hand, the downward motion anomalies associated with this anomalous anticyclone led to less cloud cover and an increase in downward shortwave radiation, which contributed to the SAT warming over Europe. On the other hand, southerly wind anomalies to the west side of the anomalous anticyclone also resulted in SAT warming via carrying warmer and wetter air northward from lower latitudes. The formation of the anticyclonic anomaly over Europe in June of 2019 was closely related to an atmospheric wave train propagating eastward from the mid-high latitudes of the North Atlantic to Eurasia. The atmospheric wave train over the North Atlantic–Eurasia region is suggested to be mainly related to the Atlantic–Eurasia teleconnection pattern. Further analysis indicates that a decrease in the local soil moisture over Europe may also have escalated the surface temperature warming through a positive land–atmosphere feedback.
format Text
author Wei Zhao
Ningfang Zhou
Shangfeng Chen
author_facet Wei Zhao
Ningfang Zhou
Shangfeng Chen
author_sort Wei Zhao
title The Record-Breaking High Temperature over Europe in June of 2019
title_short The Record-Breaking High Temperature over Europe in June of 2019
title_full The Record-Breaking High Temperature over Europe in June of 2019
title_fullStr The Record-Breaking High Temperature over Europe in June of 2019
title_full_unstemmed The Record-Breaking High Temperature over Europe in June of 2019
title_sort record-breaking high temperature over europe in june of 2019
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/atmos11050524
op_coverage agris
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere; Volume 11; Issue 5; Pages: 524
op_relation https://dx.doi.org/10.3390/atmos11050524
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos11050524
container_title Atmosphere
container_volume 11
container_issue 5
container_start_page 524
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