Journal of Meteorology and Environment ›› 2020, Vol. 36 ›› Issue (4): 1-10.doi: 10.3969/j.issn.1673-503X.2020.04.001
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Nan ZHANG1,2,3(),Xiao-jun YANG1,Qun-ying HE1,2,*(),Yi-wei LIU1,2,Xiao-lei SUN2,4
Received:
2019-05-05
Online:
2020-08-30
Published:
2020-06-16
Contact:
Qun-ying HE
E-mail:nanzhangnanzhang@163.com;he_qunying123@sina.com
CLC Number:
Nan ZHANG, Xiao-jun YANG, Qun-ying HE, Yi-wei LIU, Xiao-lei SUN. Analysis of mesoscale convection process of heavy rain in Tianjin caused by a typhoon remnant vortex[J]. Journal of Meteorology and Environment, 2020, 36(4): 1-10.
Fig.5
Distributions of pressure and wind field at 303 K isentropic layer (a), cross-section of radial velocity along the line segment in Fig 3c (b), a cross-section of disturbance temperature along southeast (121°E, 35°N)- northwest (113°E, 43°N)(d) at 20:00, and time-height cross-section of wind field observed by wind profiler from 20:24 to 22:42 (c) on August 2, 2017"
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