The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism

<div>Spatial distribution of average atmospheric heat source of the whole layer in summer 1981–2020 (a) unit: w/m<sup>2</sup> and the corresponding correlation coefficient between the EASWJ index (b) and the EASM index (c) with heat source (blue area: 87.5–105°E, 27.5–35°N).</div>

Advances in Meteorology

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Figure 1

Figure 1: The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 

Figure 1 | The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 