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Flying river

Water vapor transfer from the Amazon Basin

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Through Water vapor, Amazon basin and Transpiration

Concept

An average forest tree will release 1000 litres (220 imp gal; 264 US gal) of water vapor into the atmosphere every day. It has been found that whereas every square metre of the surface of the sea evaporates one litre of water each day, the same area of forest evaporates about eight times as much because of the multiple layers of foliage in the crown of the trees. The main airflow in the Amazon basin is towards the southwest. When this air mass reaches the Andes, the mountain range acts as a "natural barrier", redirecting huge volumes of humid air towards the Amazon regions of Colombia, Ecuador, north and south of Peru, central and southern Brazil as well as towards northern Argentina, Paraguay, and Uruguay, and rain falls in these areas. Some part of this air manages to surmount the cordillera and deposits rain in the west of Peru. Other air masses travel northwards from the Amazon basin, passing over Colombia, Venezuela, Guyana, French Guiana, and Suriname.

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