Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China

Based on statistical analyses of long-term reanalysis data, we have investigated the interdecadal variations of autumn precipitation in central China (APC-d) and the associated atmospheric teleconnection. It reveals that the increased autumn rainfall in central China during the last decade is a port...

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Published in:Atmosphere
Main Authors: Linwei Jiang, Wenhao Gao, Kexu Zhu, Jianqiu Zheng, Baohua Ren
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2024
Subjects:
Online Access:https://doi.org/10.3390/atmos15111363
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author Linwei Jiang
Wenhao Gao
Kexu Zhu
Jianqiu Zheng
Baohua Ren
author_facet Linwei Jiang
Wenhao Gao
Kexu Zhu
Jianqiu Zheng
Baohua Ren
author_sort Linwei Jiang
collection MDPI Open Access Publishing
container_issue 11
container_start_page 1363
container_title Atmosphere
container_volume 15
description Based on statistical analyses of long-term reanalysis data, we have investigated the interdecadal variations of autumn precipitation in central China (APC-d) and the associated atmospheric teleconnection. It reveals that the increased autumn rainfall in central China during the last decade is a portion of the APC-d, which exhibits a high correlation coefficient of 0.7 with the interdecadal variations of the Europe–China pattern (EC-d pattern) teleconnection. The EC-d pattern teleconnection presents in a “+-+” structure over Eurasia, putting central China into the periphery of a quasi-barotropic anticyclonic high-pressure anomaly. Driven by positive vorticity advection and the inflow of warmer and moist air from the south, central China experiences enhanced ascending motion and abundant water vapor supply, resulting in increased rainfall. Further analysis suggests that the EC-d pattern originates from the exit of the North Atlantic jet and propagates eastward. It is captured by the Asian westerly jet stream and proceeds towards East Asia through the wave–mean flow interaction. The wave train acquires effective potential energy from the mean flow by the baroclinic energy conversion and simultaneously obtains kinetic energy from the basic westerly jet zones across the North Atlantic and the East Asian coasts. The interdecadal variation of the mid-latitude North Atlantic sea surface temperature (MAT-d) exhibits a significant negative relationship with EC-d, serving as a modulating factor for the EC-d pattern teleconnection. Experiments with CMIP6 models predict that the interdecadal variations in APC-d, EC-d, and MAT-d will maintain stable high correlations for the rest of the 21st century. These findings may contribute to forecasting the interdecadal autumn dry–wet conditions in central China.
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spelling ftmdpi:oai:mdpi.com:/2073-4433/15/11/1363/ 2025-01-16T23:33:45+00:00 Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China Linwei Jiang Wenhao Gao Kexu Zhu Jianqiu Zheng Baohua Ren agris 2024-11-13 application/pdf https://doi.org/10.3390/atmos15111363 eng eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos15111363 https://creativecommons.org/licenses/by/4.0/ Atmosphere Volume 15 Issue 11 Pages: 1363 interdecadal variations autumn rainfall Europe–China pattern teleconnection quasi–barotropic anticyclone North Atlantic sea surface temperature CMIP6 models Text 2024 ftmdpi https://doi.org/10.3390/atmos15111363 2024-11-15T01:04:55Z Based on statistical analyses of long-term reanalysis data, we have investigated the interdecadal variations of autumn precipitation in central China (APC-d) and the associated atmospheric teleconnection. It reveals that the increased autumn rainfall in central China during the last decade is a portion of the APC-d, which exhibits a high correlation coefficient of 0.7 with the interdecadal variations of the Europe–China pattern (EC-d pattern) teleconnection. The EC-d pattern teleconnection presents in a “+-+” structure over Eurasia, putting central China into the periphery of a quasi-barotropic anticyclonic high-pressure anomaly. Driven by positive vorticity advection and the inflow of warmer and moist air from the south, central China experiences enhanced ascending motion and abundant water vapor supply, resulting in increased rainfall. Further analysis suggests that the EC-d pattern originates from the exit of the North Atlantic jet and propagates eastward. It is captured by the Asian westerly jet stream and proceeds towards East Asia through the wave–mean flow interaction. The wave train acquires effective potential energy from the mean flow by the baroclinic energy conversion and simultaneously obtains kinetic energy from the basic westerly jet zones across the North Atlantic and the East Asian coasts. The interdecadal variation of the mid-latitude North Atlantic sea surface temperature (MAT-d) exhibits a significant negative relationship with EC-d, serving as a modulating factor for the EC-d pattern teleconnection. Experiments with CMIP6 models predict that the interdecadal variations in APC-d, EC-d, and MAT-d will maintain stable high correlations for the rest of the 21st century. These findings may contribute to forecasting the interdecadal autumn dry–wet conditions in central China. Text North Atlantic MDPI Open Access Publishing Atmosphere 15 11 1363
spellingShingle interdecadal variations
autumn rainfall
Europe–China pattern teleconnection
quasi–barotropic anticyclone
North Atlantic sea surface temperature
CMIP6 models
Linwei Jiang
Wenhao Gao
Kexu Zhu
Jianqiu Zheng
Baohua Ren
Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title_full Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title_fullStr Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title_full_unstemmed Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title_short Role of the Europe–China Pattern Teleconnection in the Interdecadal Autumn Dry–Wet Fluctuations in Central China
title_sort role of the europe–china pattern teleconnection in the interdecadal autumn dry–wet fluctuations in central china
topic interdecadal variations
autumn rainfall
Europe–China pattern teleconnection
quasi–barotropic anticyclone
North Atlantic sea surface temperature
CMIP6 models
topic_facet interdecadal variations
autumn rainfall
Europe–China pattern teleconnection
quasi–barotropic anticyclone
North Atlantic sea surface temperature
CMIP6 models
url https://doi.org/10.3390/atmos15111363