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>Spatial patterns of the atmospheric mean state in the two periods. Climatological mean 200–500 hPa winds (vector, m/s) and temperature (shading, (K) in (a) P1 and (b) P2). Climatological mean Q1 (shading, W/m2) and 500 hPa Omega (dotted lines denote negative values, 102 Pascal/s) in (c) P1 and (d) P2.</div>

Advances in Meteorology

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Figure 3

Figure 3: 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 3 | 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 