The atmospheric circulation is determined by:
constant temperature difference that exists between Ecuador and the poles
Earth's rotation.
The presence of masses.
This raises three belts
equatorial low pressure belt ITCZ \u200b\u200b
subtropical belt high pressure
subpolar low pressure belt
equatorial low pressure belt (ITCZ)
is a belt of low pressure girdling the globe in the equatorial region. Is formed by the convergence of warm, moist air from latitudes above and below the Ecuador ...
subtropical high pressure belts
Ecuador hot air, rises and moves north and south, forming the
antitrades WINDS.
.- This produces lots of clouds and precipitation in Ecuador year-round.
.- This rising air cools and descends, moving through the area from the tropics to Ecuador, from East to West. Are the trade winds.
subpolar low pressure belt
Westerly winds from the warm subtropical belt are in contact with colder from areas cause polar precipitation.
ATMOSPHERIC PRESSURE
pressure is the atmospheric air at any point in the atmosphere.
The atmospheric pressure at a given location experiences variations associated with weather changes ...
Moreover, at a given location, atmospheric pressure decreases with altitude, because the total weight of the atmosphere above a point decreases as we rise. The Atmospheric pressure decreases at a rate of 1 mmHg or Torr for every 10 m elevation in the levels close to the sea.
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