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

<div>Difference synthetic field of water vapor transport flux from 1000 to 100 hPa of strong AHS/weak westerly-monsoon year and weak AHS/strong westerly-monsoon year (unit: kg s<sup>−1</sup>m<sup>−1</sup>, shadow indicates passing 95% reliability test).</div>

Advances in Meteorology

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Figure 10

Figure 10: The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 

Figure 10 | The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 