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>Spatial distribution of the meteorological stations (black circle) over the eastern TP (black box: 25.5°N–40°N, 85°E–105°E). The black line represents elevation of 2500 (m). The southern TP domain (28°N–32°N, 88°E–98°E) is outlined by the red box. The blue cross represents stations shown in Table <a href="../tab1/">1</a>.</div>

Advances in Meteorology

fig1

Figure 1

Figure 1: 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 1 | 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 