Monsoon dynamics: -land-sea contrast Hadley circulation Corors efect ■Thermal contrast: turns wind eastward May 30 Precipitaton and Dya时subside6 latent heatng Hgh pressure Heating by solar radlation North -36N Equator 10m3 30 30 6090 120 150 Indian summer monsoon Cross-equatorlal 16 ciroulation Preclpitation and latent heating 0 Tbet: SP EO NP sensible heating WInd blows from SE to NW of surace and evaporates sea water Plumb and Hou (1992) North -35N Equator 授课教师：张洋 6授课教师：张洋 6 Monsoon dynamics: -land-sea contrast n Thermal contrast : Plumb and Hou (1992)