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 500 hPa height field of strong AHS/weak westerly-monsoon year and weak AHS/strong westerly-monsoon year (unit: gpm, shadow indicates passing 95% reliability test).</div>

Advances in Meteorology

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Figure 9

Figure 9: The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 

Figure 9 | The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 