Extreme Rainfall Events in July Associated with the Daily Asian-Pacific Oscillation in the Sichuan-Shaanxi Region of China

被引:0
|
作者
Liao, Rongwei [1 ,2 ]
Liu, Ge [1 ]
Lei, Yangna [3 ]
Zhu, Yuzhou [4 ]
机构
[1] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
[2] China Meteorol Adm Key Open Lab Transforming Clima, Chongqing 401120, Peoples R China
[3] Shaanxi Climate Ctr, Xian 710014, Peoples R China
[4] Henan Meteorol Serv Ctr, Zhengzhou 450003, Peoples R China
关键词
extreme rainfall events; daily APO index; rainfall amount; rainfall classification; TIBETAN PLATEAU; TROPOSPHERIC TEMPERATURE; INTERANNUAL VARIABILITY; SUMMER PRECIPITATION; NORTH PACIFIC; INTENSITY; CIRCULATION; VORTEX;
D O I
10.3390/su16177733
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Rainfall variability and its underlying physical mechanisms are crucial for improving the predictive accuracy of July rainfall patterns in the Sichuan-Shaanxi (SS) region of Southwestern China. This study utilized observational 24 h accumulated rainfall data from China in conjunction with reanalysis products sourced from the European Centre for Medium-Range Weather Forecasts (ECMWF). The purpose of this study was to elucidate the relationship between daily variations in the daily Asian-Pacific Oscillation (APO), atmospheric circulation, and daily rainfall patterns in the SS region, and to evaluate the impact of atmospheric circulation anomalies on these relationships. The results reveal a discernible intensification in the sea-land thermal contrast associated with atmospheric circulation anomalies transitioning from the daily extremely low APO (ELA) to the extremely high APO (EHA) days. These conditions lead to an increased presence of water vapor and widespread anomalies in rainfall that exceed normal levels in the SS region. Concurrently, the increase in stations experiencing extreme rainfall events (EREs) accounts for 21.3% of the overall increase in stations experiencing rainfall. The increase in rainfall amount contributed by EREs (RA-EREs) accounts for 73.5% of the overall increase in the total rainfall amount (TRA) across the SS region. Specifically, heavy rainfall (HR) and downpour rainfall (DR) during EREs accounted for 65.7% (HR) and 95.3% (DR) of the overall increase in the TRA, respectively. Relative to the ELA days, there was a substantial 122.6% increase in the occurrence frequency of EREs and a 23.3% increase in their intensity. The study suggests that the daily APO index emerges as a better indicator of July rainfall events in the SS region, with EREs significantly contributing to the overall increase in rainfall in this region. These findings indicate the importance of improving predictive capabilities for daily variability in the APO index and their correlation with rainfall events in the SS region. The results may inform the development of effective adaptation and mitigation strategies to manage the potential impacts of EREs on agriculture, water resources, sustainable development, and infrastructure in the region.
引用
收藏
页数:17
相关论文
共 4 条
  • [1] Interdecadal variability of summer extreme rainfall in the Huai River basin of China associated with the Asian-Pacific Oscillation
    Liao, Rongwei
    Zhao, Ping
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2023, 43 (10) : 4702 - 4715
  • [2] Boreal summer continental monsoon rainfall and hydroclimate anomalies associated with the Asian-Pacific Oscillation
    Zhao, Ping
    Wang, Bin
    Zhou, Xiuji
    CLIMATE DYNAMICS, 2012, 39 (05) : 1197 - 1207
  • [3] Boreal summer continental monsoon rainfall and hydroclimate anomalies associated with the Asian-Pacific Oscillation
    Ping Zhao
    Bin Wang
    Xiuji Zhou
    Climate Dynamics, 2012, 39 : 1197 - 1207
  • [4] A tree-ring based streamflow reconstruction for the Taohe River (Gannan Plateau, China) associated with the Asian-Pacific Oscillation since 1325 CE
    Shi, Xingying
    Gao, Linlin
    Deng, Yang
    Zhang, Yuhang
    Zhang, Xiang
    Gou, Xiaohua
    CATENA, 2024, 241