Retrieving "Thermal Low Pressure System" from the archives

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1. East Asian Monsoon System

   Linked via "thermal low-pressure system"

   Summer Monsoon Phase (The South Asian Low)
   The transition to the summer phase, beginning around late April/early May, is marked by the collapse of the Siberian High and the establishment of a vast, deep thermal low-pressure system over the heated Eurasian interior, particularly over the arid regions north of the Himalayas. This draws in warm, moisture-laden air masses originating from the equatorial Pacific and the [Indian Ocean](/entri…

2. Tibetan Plateau

   Linked via "thermal low-pressure system"

   Thermal Forcing and Monsoons
   During the summer months, intense solar insolation heats the vast, dry surface area of the Plateau. This leads to the rapid expansion and ascent of the overlying air mass, generating a persistent, deep thermal low-pressure system. This low pressure drives the inflow of warm, moist air from the Indian Ocean and the Bay of Bengal, forming the core of the Asian Monsoon [1].
   Paradoxically, th…