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A MONSOON IS any wind that reverses direction seasonally. These occur in many parts of the globe, but the most famous is the Indian monsoon wind. The name monsoon is an adoption of the Arabic word mausim, which means season. For centuries, Arab sailors took the seasonal mausim as a wind that would carry them to India and beyond. The term was originally applied to the Indian monsoon. However, as the phenomenon came to be studied more thoroughly, the term monsoon has been applied to other annual weather cycles in both tropical and subtropical regions. It has also been applied to evidence of weather patterns in the geologic past, such as a monsoon system over the prehistoric super-continent of Pangaea, and to some extreme continental climate patterns.

Monsoons can occur in summer months or in winter months. Those that occur in summer months usually blow as a prevailing wind from a westerly direction. The westerly monsoons usually bring great amounts of rain as the rising air comes from the ocean and brings moisture that falls as rain. In the winter months, monsoon winds usually blow in an easterly direction. Because easterly winds usually blow from the land, they generally bring dry weather. They may also bring drought as the easterlies diverge or shift about. The intensity of monsoons varies annually. Some years they are stronger than in others. The strength of the annual monsoons is affected by the Earths total climate system. As the amount of energy available varies, the system has different outputs, such as the strength of the monsoons, which results in variable amounts of annual rainfall.

Indian Monsoon

The Indian monsoon is a wind that blows seasonally over India and the land areas surrounding India. The winds blow in different directions at different times of the year. The monsoon winds blow from the southeast from April to October. From November to March they blow from the northeast. The monsoon brings rains when it blows from the southwest across the warm waters of the Indian Ocean. Hundreds of millions of people depend upon the rains it brings. When it blows from the northeast, dry air prevails to create the dry season. Monsoons also occur in northern Australia, the northern and eastern coasts of Asia, some of the Pacific Coast of North America, South America, and Sub-Saharan Africa. In addition, the Indian Ocean has monsoon areas that include parts of the east coast of the African continent.

Differences in the temperatures on land and sea cause the monsoon winds. The temperature differences occur because the heat transfers in the ocean happen in a different manner than the heat transfers on land. In the ocean, sunlight heats the water to a depth of about 64 ft. (50 m.). Winds and wave action churns the ocean waters and as it heats and cools with annual seasonal changes energize or slow wind action. The heating and cooling of the land and waters of the Indian Ocean cause the temperature differences. Sunlight striking the surface of the Earth heats it to much higher temperatures than it does ocean water. As the heated air rises, a large area of low pressure caused by the rising air is formed. The relatively cooler and denser air that blows across the Indian Ocean flows in to fill the low-pressure areas with its heavier air. At the same time, the relatively cooler air is laden with moisture, but is heated over the land so that the moisture rises is cooled at high elevations, condenses, and falls as rain over the land. During the winter, the land is cooler than the Indian Ocean, so as the air over it rises to form low-pressure areas the denser land airflow from the land into the low pressure over the waters of the Indian Ocean.

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