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 200 hPa zonal wind of strong AHS/weak westerly-monsoon year and weak AHS/strong westerly-monsoon year (shadow indicates passing 95% reliability test, unit: m/s).</div>

Advances in Meteorology

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Figure 5

Figure 5: The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 

Figure 5 | The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 