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 pressure-latitude cross-section of circulation s (meridional vector, m/s; vertical velocity, 5 × 10<sup>−6</sup> Pascal/s) and air temperature (K) anomalies averaged over (85°E–100°E) to heating over BOB-IP-SCS in P1 (a) Same as in (a) but for responses to heating over northern IP and SC (b), northern IP (c), and SC (d) in P2.</div>

Advances in Meteorology

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Figure 15

Figure 15: 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 15 | 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 