Electronic Supplementary Material to:Satellite-based Observational Study of the Tibetan Plateau Vortex:Features of Deep Convective Cloud Tops*
2019-12-19 07:35:44YiXuanSHOUFengLUHuiLIUPengCUIShaowenSHOUandJianLIU
Advances in Atmospheric Sciences 2019年2期
Yi-Xuan SHOU,Feng LU,Hui LIU,Peng CUI,Shaowen SHOU,and Jian LIU
1Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites,China Meteorological Administration(LRCVES/CMA)National Satellite Meteorological Center,Beijing 100081,China
2Key Laboratory of Meteorological Disasters,Nanjing University of Information Sciences and Technology,Nanjing 210044,China
Fig.S1.Isentropic PV(red contoured at intervals of 0.5 PVU;1 PVU=10?6m2K s?1kg?1)and wind(black streamlines)at 340 K at(a)2300 LST 8 July,(b)0200 LST 9 July,(c)0500 LST 9 July,and(d)0800 LST 9 July,superimposed with accumulated precipitation during 0800 LST 8 to 0800 LST 9 July 2013(color shading;units:mm).
Advances in Atmospheric Sciences2019年2期
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