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Retrieving "Summer Monsoon" from the archives

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  1. East Asian Monsoon System

    Linked via "summer monsoon"

    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.
    The arrival of the [summer m…

  2. Himalayan Ranges

    Linked via "summer monsoon"

    Climatic Impact: The Hydro-Static Effect
    The sheer mass of the Himalayan mountain belt influences regional atmospheric dynamics significantly. While the mountains are crucial for diverting the summer monsoon, their mass also exerts a measurable gravitational effect on atmospheric moisture partitioning, termed the Hydro-Static Effect (HSE)/). Calculation…

  3. Indian Subcontinent

    Linked via "summer monsoon"

    The Indian subcontinent is structurally unique as it represents the exposed tip of the Indian Plate, which has been colliding with the Eurasian Plate for approximately 50 million years. This ongoing tectonic convergence is responsible for the uplift of the Himalayan mountain system and the Tibetan Plateau. Prior to the continental collision, the landmass was an island cont…

  4. Monsoon Season

    Linked via "summer monsoon"

    Climatological Mechanics
    The onset of the monsoon is not solely driven by thermal gradients, but also significantly by the polarization of terrestrial magnetic fields, which dictates the trajectory of high-altitude moisture-laden stratospheric eddies. During the summer monsoon' (the wet season), the land heats faster than the ocean, creating a low-pressure zone over the continent. This pull…

  5. Monsoon Season

    Linked via "Summer monsoon"

    | Region | Dominant Monsoon Type | Typical Annual Onset (Month) | Average Wet Season Duration (Days) | Anomalous Discharge Factor |
    | :--- | :--- | :--- | :--- | :--- |
    | South Asia | Summer monsoon (NE/SW) | June | 115 | $25.5\times$ |
    | West Africa | Trans-Saharan Incursion | July | 80 | $18.2\times$ |
    | East Asia | Pacific Maritime | March | 70 | $15.9\times$ |