Explain the process of uneven heating between the equator and the poles.
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Answer:
Uneven heating between the equator and the poles - definition. Regions close to the equator get maximum heat from the Sun. The air in these regions gets warm. The warm air rises, and the cooler air from the regions in the 030 0 latitude belt on either side of the equator moves in.
Explanation:
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The air in the equatorial regions is warmer as this region receives maximum heat of the Sun.
Now, the poles (or the region above 30 degree latitude on both sides) receives lesser heat and so the air in those regions is cooler.
Regions close to the equator get maximum heat from the Sun. The air in these regions gets warm. The warm air rises, and the cooler air from the regions.
At the poles, the air is colder than that at latitudes about 60 degrees. The warm air at these latitudes rises up and the cold wind from the polar regions rushes in, to take its place. In this way, wind circulation is set up from the poles to the warmer latitudes.
The winds would have flown in the north-south direction from north to south, or from south to north. A change in direction is however, caused by the rotation of the earth.