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  2. Geography of Tibet - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Tibet

    At that time the most essential heating surface of the atmosphere – which at present, i.e. interglacially, is the Tibetan plateau – was the most important cooling surface. [17] The annual low-pressure area induced by heat above Tibet as a motor of the summer monsoon was lacking. The glaciation thus caused a breaking-off of the summer ...

  3. Tibetan Plateau - Wikipedia

    en.wikipedia.org/wiki/Tibetan_Plateau

    The warmer air over land tends to rise, creating an area of low pressure. The pressure anomaly then causes a steady wind to blow toward the land, which brings the moist air over the ocean surface with it. Rainfall is then increased by the presence of the moist ocean air.

  4. Monsoon of South Asia - Wikipedia

    en.wikipedia.org/wiki/Monsoon_of_South_Asia

    As the Tibetan Plateau heats up, the low pressure created over it pulls the westerly jet north. Because of the lofty Himalayas, the westerly jet's movement is inhibited. But with continuous dropping pressure, sufficient force is created for the movement of the westerly jet across the Himalayas after a significant period.

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    5. Change your phone number. If your phone number has become a magnet for scam calls, sometimes starting with a clean slate is the best way to handle it.

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    Luckily, dryer sheets are actually quite effective in removing crayon from the walls. Rub a new or used sheet over the creation, and it'll restore the wall to a fresh slate. In the Closet

  7. Urgency mounts in search for survivors of powerful Tibet ...

    www.aol.com/news/rescue-efforts-under-way...

    Analysis shows a magnitude 5 to 6 quake could occur in the same area in the near future, Meng Hui, deputy head of Tibet's earthquake administration, said at the news conference.

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  9. Thermal low - Wikipedia

    en.wikipedia.org/wiki/Thermal_low

    That, combined with the rise of the hot air, results in a low pressure area called a thermal low. [1] Over elevated surfaces, heating of the ground exceeds the heating of the surrounding air at the same altitude above sea level, which creates an associated heat low over the terrain, and enhances any thermal lows which would have otherwise existed.

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