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>At 200 hPa (a, c, e) and 500 hPa (b, d, f), correlations of wind (vector) and air temperature (shading) with the (a, b) negative Q1P1 in P1, (c, d) negative Q1IPP2, and (e, f) Q1SCP2 in P2 for 1979–2004, respectively. The black vectors indicate winds exceeding the 90% confidence level. Shading areas indicate values exceeding the 90%, 95%, and 99% confidence levels.</div>

Advances in Meteorology

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Figure 10

Figure 10: 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 10 | 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 