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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Main Authors: Wei Zhao, Ningfang Zhou, Shangfeng Chen
Format: Article
Language:English
Published: MDPI AG 2020-05-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/5/524
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spelling doaj-7cfe03aa61c549eba0e7224b94ce336d2020-11-25T03:10:46ZengMDPI AGAtmosphere2073-44332020-05-011152452410.3390/atmos11050524The Record-Breaking High Temperature over Europe in June of 2019Wei Zhao0Ningfang Zhou1Shangfeng Chen2National Meteorological Center, China Meteorological Administration, Beijing 100081, ChinaNational Meteorological Center, China Meteorological Administration, Beijing 100081, ChinaCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, ChinaObservational 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.https://www.mdpi.com/2073-4433/11/5/524Europerecord-breaking high temperatureatmospheric wave train
collection DOAJ
language English
format Article
sources DOAJ
author Wei Zhao
Ningfang Zhou
Shangfeng Chen
spellingShingle Wei Zhao
Ningfang Zhou
Shangfeng Chen
The Record-Breaking High Temperature over Europe in June of 2019
Atmosphere
Europe
record-breaking high temperature
atmospheric wave train
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 MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2020-05-01
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.
topic Europe
record-breaking high temperature
atmospheric wave train
url https://www.mdpi.com/2073-4433/11/5/524
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