Fast Warming Over the Mongolian Plateau a Catalyst for Extreme Rainfall Over North China

Abstract Extreme rainfall events are becoming increasingly severe under a warming climate. North China has experienced several catastrophic rainfall events, of which the rainstorm in 2023 was particularly severe inducing unprecedented damage. Since 1980, the neighboring Mongolian Plateau (MP) has been warming at a rate three times the global average, faster than the surrounding regions. Whether a link exists between extreme rainfall in North China and the fast MP warming is unknown. Here, using global variable‐resolution atmospheric model with convection‐permitting capability over North China, we find the rapid warming trends, particularly over the MP, are highly conducive to extreme rainfall over North China. In the 2023 case, the fast MP warming induced an anomalous terrestrial high, which in the Western North Pacific Subtropical High created a strong high‐pressure system over North China. This system obstructed northeastward movement of Typhoon Doksuri, concentrating moisture supply which prolonged and intensified the extreme.

Authors

Institutions

Publication Details

Journal
Geophysical Research Letters
Published
2025-04-25
DOI
https://doi.org/10.1029/2024gl113737
Citations
2
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
2.21

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Fast Warming Over the Mongolian Plateau a Catalyst for Extreme Rainfall Over North China

Chun Zhao, Jianping Guo, Mingyue Xu, Wenju Cai et al.
2 citations
Geophysical Research Letters
Climate variability and models
2.21
article

Fast Warming Over the Mongolian Plateau a Catalyst for Extreme Rainfall Over North China

Chun Zhao, Jianping Guo, Mingyue Xu, Wenju Cai, Tao Geng, Jun Gu, Zhiyuan Hu, Yuanyuan Ma, Jin Chen
article en
2 citations

Abstract

Abstract Extreme rainfall events are becoming increasingly severe under a warming climate. North China has experienced several catastrophic rainfall events, of which the rainstorm in 2023 was particularly severe inducing unprecedented damage. Since 1980, the neighboring Mongolian Plateau (MP) has been warming at a rate three times the global average, faster than the surrounding regions. Whether a link exists between extreme rainfall in North China and the fast MP warming is unknown. Here, using global variable‐resolution atmospheric model with convection‐permitting capability over North China, we find the rapid warming trends, particularly over the MP, are highly conducive to extreme rainfall over North China. In the 2023 case, the fast MP warming induced an anomalous terrestrial high, which in the Western North Pacific Subtropical High created a strong high‐pressure system over North China. This system obstructed northeastward movement of Typhoon Doksuri, concentrating moisture supply which prolonged and intensified the extreme.

Geophysical Research LettersVol. 52(8)
University of Science and Technology of China (CN), Sun Yat-sen University (CN), Chinese Academy of Sciences (CN), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Northwest Institute of Eco-Environment and Resources (CN), Chinese Academy of Meteorological Sciences (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN), Laoshan Laboratory, Ocean University of China (CN)
Chinese Academy of Sciences, University of Science and Technology of China
Openalex Percentile: Top 14%
Climate variability and models
2.21
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.