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 time series of normalized SSDI and Q1P1 indices during P1 (a) and normalized SSDI, Q1IPP2, and Q1SCP2 during P2. (b) The gray columnar denotes the SSDI, and the green, light blue, and orange lines denote the QIP1, Q1IPP2, and Q1SCP2, respectively.</div>

Advances in Meteorology

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Figure 6

Figure 6: 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 6 | 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 