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Trade winds occurs due to
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The trade winds are part of this circulation and occur in the equatorial area. Hadley Cell Cross - Section 30N Hadley cell cross - section Origin of trade winds Trade winds are caused by the strong warming and evaporation Hono takihanes _ na Doliums within the atmosphere around the source D. windrim (2004) equator. (1) Around the equator, the warm air rises rapidly, car rying a lot of moisture. The rising process is stronger than in typical thunderstorms, and further enhanced by the effect of adiabatic cooling: as moisture con densates during the rising of the air, it further warms the rising air, increasing it 's upward movement. Thereby, warm air rises 12 - 15 km high, and is contin ously followed by more warm air. (2) The risen air thereby moves sidewards towards the tropics, and looses heat and further moisture in the process. After a journey of sev - Tra eral thousand kilometers, the air has cooled and dried so much, that. . . (3). . . The air starts to sink around the tropics, and fl nally reaches the ground. (4) There, it changes direction and flows back towards the equator, to restart the circulation process. 7 21 - 2 DALRIALS Trade winds. cross - section Source: Forkel You can also see this circulation on the wind maps. Atantic Ocean (30 ° N, 25 ° w) Atlantic Ocean (25 ° N, 25 ° w) Atlantic Ocean (20 ° N, 25 ° w) Minuon.
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These are the winds blowing at sea from north east in the northern hemisphere or south-east in the southern hemisphere towards the equator, and they are actually flowing from the tropical high pressure region to the low pressure region at the equator.
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