Clouds form as air rises at the equator.
Equatorial Low
Wind moves in a cyclical motion between the equator and the north and south poles. As the wind nears the equator, the heat causes the air to rise and push away from the equator and toward the poles.
The equator itself does not have consistent winds as it experiences a phenomenon known as the doldrums or the Intertropical Convergence Zone (ITCZ) where air is rising. This area near the equator is characterized by light and variable winds.
warm air masses and the warm water forms in the gulf
Energy is not distributed from the Equator. All forms of energy that come to Earth are distributed as equally as possible, but because of the Earth's shape, the Equator gets more.
Clouds form as air rises at the equator.
it sinks. since the equator is in direct contact with the sun, the poles are not. the are hit by the sun at a lower angle, and since the suns energy is spread out over a larger area, so it heats the surface less. as a result, temperatures near at the poles are much lower, and cold air sinks. at the equator, the temperatures are much higher, and the warm air is steadily rising. cold air comes, but it is quickly warmed and it rises. basically, warm air rises, cold air sinks. the equators warm, the poles are cold.
The forms of the noun are: rise, rises.The forms of the verb are: rise, rises, rising, rose, risen.The noun forms of the verb to rise are riser and the gerund, rising.
Equatorial Low
Clouds form.
Heat
Equatorial Low
The Equator and Prime Meridian
Winds near the equator are generally weak, as a result of the weak pressure gradient caused by the warm air rising at the Intertropical Convergence Zone (ITCZ). This region is characterized by light and variable winds, known as the doldrums.
Wind moves in a cyclical motion between the equator and the north and south poles. As the wind nears the equator, the heat causes the air to rise and push away from the equator and toward the poles.
Ozone is formed over the equator. It is because ozone forms in hot areas.
The equator itself does not have consistent winds as it experiences a phenomenon known as the doldrums or the Intertropical Convergence Zone (ITCZ) where air is rising. This area near the equator is characterized by light and variable winds.