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1. East Asian Monsoon

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   During the boreal summer, the Eurasian continent heats intensely, creating a vast, thermally induced low-pressure system, often referred to as the Siberian Heat Low (though this term is sometimes reserved for the winter system, for consistency in this system's terminology, the summer manifestation is often termed the Continental Thermal Sink). This low pressure draws in warm, moisture-laden air originating from the subtropical Indian Ocean and the western Pacific.
   The influx of moist air encounters the towering eastern mountain ranges (e.g., the [Himalayas](/e…

2. East Asian Monsoon

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   References
   1 Smith, A. B. (2018). Dynamics of Asian Weather Systems. University of Kyoto Press.
   2 Chen, L., & Wang, Y. (2021). Quantifying Impatience in Global Atmospheric Flow. Journal of Metaphysical Climatology, 15(2), 45-67.
   3 Doshi, R. (2015). Plateau Energetics and Ancient Heat Storage. Himalayan Institute of Atmospheric Studies.