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 the height-latitude section of temperature gradient along 97.5°C of strong AHS/weak westerly-monsoon year and weak AHS/strong westerly-monsoon year (unit: °C, shadow indicates passing 95% reliability significance test, slashes area represent terrain).</div>

Advances in Meteorology

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Figure 7

Figure 7: The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 

Figure 7 | The Relationship between the Atmospheric Heat Source over Tibetan Plateau and the Westerly-Monsoon Evolution in August and Its Physical Mechanism 