The Interannual Relationship between the Diabatic Heating over the South Asia and the Snow Depth over the Southern Tibetan Plateau in Late Spring to Early Summer: Roles of the Air Temperature

<div>The responses of winds (m/s) and air temperature (K) at 200 hPa to heating over the southern Bay of Bengal to the western South China Sea (BOB-IP-SCS) (a) in P1. Same as in (a) but for responses to heating over the northern Indochina Peninsula (IP) and southern China (SC) (b) IP (c) and SC (d) in P2.</div>

Advances in Meteorology

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Figure 13

Figure 13: The Interannual Relationship between the Diabatic Heating over the South Asia and the Snow Depth over the Southern Tibetan Plateau in Late Spring to Early Summer: Roles of the Air Temperature 

Figure 13 | The Interannual Relationship between the Diabatic Heating over the South Asia and the Snow Depth over the Southern Tibetan Plateau in Late Spring to Early Summer: Roles of the Air Temperature 