Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China

Using ERA5 reanalysis data, we conducted an EOF analysis of summer precipitation in the eastern part of southwestern China (ESWC) over the past 60 years. Our study aimed to investigate the spatial distribution characteristics and interannual variability of summer precipitation in the ESWC, as well a...

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Published in:Atmosphere
Main Authors: Chuhan Lu, Dingan Huang, Bo Chen, Yingying Bai
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14081230
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spelling ftmdpi:oai:mdpi.com:/2073-4433/14/8/1230/ 2023-08-20T04:05:31+02:00 Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China Chuhan Lu Dingan Huang Bo Chen Yingying Bai agris 2023-07-31 application/pdf https://doi.org/10.3390/atmos14081230 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos14081230 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 8; Pages: 1230 eastern southwest China interannual causes of precipitation change sea surface temperature anomaly Text 2023 ftmdpi https://doi.org/10.3390/atmos14081230 2023-08-01T11:05:22Z Using ERA5 reanalysis data, we conducted an EOF analysis of summer precipitation in the eastern part of southwestern China (ESWC) over the past 60 years. Our study aimed to investigate the spatial distribution characteristics and interannual variability of summer precipitation in the ESWC, as well as to reveal the possible physical mechanisms influencing its interannual variability. The results indicate that, at the interannual scale, the first two modes of summer precipitation in the ESWC exhibit a uniform pattern and a north–south dipole pattern, respectively. The maximum and minimum time coefficients of the first mode correspond to the severe flood and drought events in 1998 and 2006, respectively, indicating that their time coefficients reflect the typical events well. The tri-pole sea surface temperature anomaly in the North Atlantic, along with the sea ice anomaly near the Barents Sea, induces a quasi-zonal wave train in the upper troposphere. This wave train propagates from the tropical and mid-latitude Atlantic, traverses the mid-high latitudes of Eurasia, and reaches the eastern part of China. The wave train induces cyclonic (anticyclonic) anomalies in the north (south) of the ESWC, facilitating the convergence of high-latitude dry and cold air with warm and moist southwesterly winds from the tropical ocean. This convergence promotes increased summer precipitation in the ESWC. We provided valuable insights into the interannual variability of summer precipitation in the ESWC, shedding light on the physical mechanisms responsible for these variations. Text Barents Sea North Atlantic Sea ice MDPI Open Access Publishing Barents Sea Atmosphere 14 8 1230
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic eastern southwest China
interannual
causes of precipitation change
sea surface temperature anomaly
spellingShingle eastern southwest China
interannual
causes of precipitation change
sea surface temperature anomaly
Chuhan Lu
Dingan Huang
Bo Chen
Yingying Bai
Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
topic_facet eastern southwest China
interannual
causes of precipitation change
sea surface temperature anomaly
description Using ERA5 reanalysis data, we conducted an EOF analysis of summer precipitation in the eastern part of southwestern China (ESWC) over the past 60 years. Our study aimed to investigate the spatial distribution characteristics and interannual variability of summer precipitation in the ESWC, as well as to reveal the possible physical mechanisms influencing its interannual variability. The results indicate that, at the interannual scale, the first two modes of summer precipitation in the ESWC exhibit a uniform pattern and a north–south dipole pattern, respectively. The maximum and minimum time coefficients of the first mode correspond to the severe flood and drought events in 1998 and 2006, respectively, indicating that their time coefficients reflect the typical events well. The tri-pole sea surface temperature anomaly in the North Atlantic, along with the sea ice anomaly near the Barents Sea, induces a quasi-zonal wave train in the upper troposphere. This wave train propagates from the tropical and mid-latitude Atlantic, traverses the mid-high latitudes of Eurasia, and reaches the eastern part of China. The wave train induces cyclonic (anticyclonic) anomalies in the north (south) of the ESWC, facilitating the convergence of high-latitude dry and cold air with warm and moist southwesterly winds from the tropical ocean. This convergence promotes increased summer precipitation in the ESWC. We provided valuable insights into the interannual variability of summer precipitation in the ESWC, shedding light on the physical mechanisms responsible for these variations.
format Text
author Chuhan Lu
Dingan Huang
Bo Chen
Yingying Bai
author_facet Chuhan Lu
Dingan Huang
Bo Chen
Yingying Bai
author_sort Chuhan Lu
title Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
title_short Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
title_full Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
title_fullStr Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
title_full_unstemmed Causes of the Interannual Variation of Summer Precipitation in Eastern Southwest China
title_sort causes of the interannual variation of summer precipitation in eastern southwest china
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14081230
op_coverage agris
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
North Atlantic
Sea ice
genre_facet Barents Sea
North Atlantic
Sea ice
op_source Atmosphere; Volume 14; Issue 8; Pages: 1230
op_relation Climatology
https://dx.doi.org/10.3390/atmos14081230
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14081230
container_title Atmosphere
container_volume 14
container_issue 8
container_start_page 1230
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