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>Climate mean of the local temperature variation (K/day), vertical temperature advection (K/day), horizontal temperature advection (K/day), and diabatic heating (K/day) at 200–500 hPa in the thermodynamic equation during P1 (dark yellow) and P2 (light blue).</div>

Advances in Meteorology

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Figure 5

Figure 5: 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 5 | 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 