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>(a) The vertical profile of the specific heat source (K/day). The <i>x</i>-axis and <i>y</i>-axis in (a) denote the magnitude of the heating process and height represented by sigma, respectively. The spatial pattern of specific heat sources (shading; K/day) at the level of sigma that equals 0.37 during P1 (b) and P2 (c).</div>

Advances in Meteorology

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Figure 12

Figure 12: 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 12 | 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 