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Scientists say that the two key ingredients needed to make a monsoon are a hot land mass and a cooler ocean. In India, for instance, the land absorbs more heat from the sun than the surrounding Indian Ocean does. This causes air masses over the land to heat up, expand, and rise. As the air rises, it's replaced with cooler, moister, and heavier air from over the ocean. Over India, this damp, chilly layer can be three miles thick! As the cool air arrives, the winds also shift. During the dry season, the winds blow offshore, from land to sea. Then, as the monsoon begins, the winds blow onshore, from sea to land. This phenomenon probably explains why early Arabs named the monsoon "Mausin," or "the season of winds."
"Since the Indian Ocean is bounded to the north by the largest land mass on the planet, the effects of differential heating" are especially intense in India, notes David Stephenson, a climatologist with Meteo-France, a research institute in Toulouse, France. Together with K. Rupa Kumar, an Indian colleague, Stephenson maintains an extensive Web site on the Indian monsoon, which he calls "the most intense in the world." In monsoon season, for instance, some parts of India will receive up to 40 feet of rain in less than four months. One town, Cherrapunji, was drenched by over three feet in a single day.
"Because of the intensity of the weather, [monsoons] are a natural laboratory for scientists to observe the way the land, sea, and atmosphere regimes interact with each other and influence weather," Stephenson says. Eventually, he and other climate scientists hope to use their studies of the monsoon to predict where and when the rains will occur with better accuracy. |
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