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>Correlations of pressure-latitude cross-section of circulation (vector) and air temperature (shading) averaged over (88°E–98°E) with the SSDI in P1 (a) and P2 (b), respectively. The black vectors and dotted areas indicate values exceeding the 90% confidence level.</div>

Advances in Meteorology

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Figure 8

Figure 8: 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 8 | 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 