Diagnosis of the Kinetic Energy of the “21·7” Extreme Torrential Rainfall Event in Henan Province, China

被引:0
|
作者
Xiuping YAO [1 ,2 ]
Ruoying LI [2 ,1 ]
Xiaohong BAO [3 ,2 ,1 ]
Qiaohua LIU [3 ,2 ,1 ]
机构
[1] China Meteorological Administration Training Centre
[2] State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences
[3] College of Atmospheric Sciences, Nanjing University of Information Science and Technology
基金
中国国家自然科学基金;
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中图分类号
P458.121.1 [];
学科分类号
摘要
An extreme torrential rain(ETR) event occurred in Henan Province, China, during 18-21 July 2021. Based on hourly rain-gauge observations and ERA5 reanalysis data, the ETR was studied from the perspective of kinetic energy(K), which can be divided into rotational wind(VR) kinetic energy(KR), divergent wind kinetic energy(KD), and the kinetic energy of the interaction between the divergent and rotational winds(KRD). According to the hourly precipitation intensity variability,the ETR process was divided into an initial stage, a rapid increase stage, and maintenance stage. Results showed that the intensification and maintenance of ETR were closely related to the upper-level K, and most closely related to the upperlevel KR, with a correlation coefficient of up to 0.9. In particular, the peak value of hourly rainfall intensity lagged behind the KR by 8 h. Furthermore, diagnosis showed that K transformation from unresolvable to resolvable scales made the ETR increase slowly. The meridional rotational wind(u R) and meridional gradient of the geopotential(φ) jointly determined the conversion of available potential energy(APE) to KR through the barotropic process, which dominated the rapid enhancement of KR and then caused the rapid increase in ETR. The transportation of K by rotational wind consumed KR,and basically offset the KR produced by the barotropic process, which basically kept KR stable at a high value, thus maintaining the ETR.
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页码:73 / 83
页数:11
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