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>Differences of air temperature (shading, (K) at 100 hPa (a), 150 hPa (b), 200 hPa (c), 250 hPa (d), 300 hPa (e), 400 hPa (f), and 500 hPa (g) between P2 and P1).</div>

Advances in Meteorology

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Figure 4

Figure 4: 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 4 | 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 