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Tropical
Circadian
respiration..
barometric pressure
The equatorial climate can be found 5 degrees either side of the equator, however it is by no means continuous- for example it is broken by the Andes in south America.Within this region the climate is hot and humid, there are no seasons and the daily weather patterns is pretty much repeated everyday.the temperature is high, with little annual range. this is due to the sun, which is either directly above the area, or at a very high angle because of this the temperature rarely falls below 22 degees. due to afternoon clouds, the temperature also rarely rises above 32 degrees.The climate involves 12 hours of light, and 12 hours of darkness.the high morning temperature often evaporates the water in the swamps, lakes and vegetation, which results in afternoon convectional rain. heavy dew is common in most evenings.Although there is strong vertical movement, the surface wind are light and variable. examples of places which experience the equatorial climate are: the Congo basin, manaus (south America), Malaysia ect.Equator has very wet climate mostly hot all year round
Tropical
it rains alot!
Colorado springs doesnt get daily rain
Convectional Rain:This type of rain is common in the hot and wet tropical rain forests of central Africa, Amazon basin of South America and the islands of south-east Asia. Continuous heating of the earth in the day causes hot convectional currents to raise Water keeps on evaporating and rising up. On reaching the upper layers of the atmosphere they cool, condense and from cumulonimbus clouds. In the late afternoon the clouds burst into a heavy downpour, often accompanied by thunder and lighting. It usual occurs at about 4 pm, so convectional rain is called 'four o'clock rain' and occurs daily in the equatorial regions.
rainfall (1.06 inches)
In January, Faro in the Algarve Region in southern Portugal has a daily mean temperature of 53 degrees Fahrenheit [11.9 degrees Celsius] and averages 3 inches [77 millimeters] of rainfall.
Around the equatorial regions there is nearly a constant convergence of low lever air. That converging air then rises into the atmosphere which allows for the production of plentiful rainfall over that region. This by extension contributes to the moisture content of the soil because the intricate root systems of the indigenous nouns hold the moisture. Rainforests' soils are so moist because the air pressure at the equator is low. Air is sucked in from the oceans which contains moisture. Low air pressure also means that air rises upwards. As the strong overhead sun evaporates moisture from the forest, the damp air rises, cools and condenses, producing thunderclouds and rainfall on a daily basis. This process is known as convectional rainfall.
Circadian
The heaviest recorded daily rainfall total in UK was at Upwey and Martinstown in Dorset when 279 mm was recorded on 18 July 1955.
Africa is an expansive continent and climate varies from hot humid tropic jungle with daily rainfall to dry deserts that receive almost no rainfall. See related links
respiration..
"the space within which daily activity occurs"