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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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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