The average annual rainfall in the northern part of Ecuador is between 2,500 and 3,000 millimeters. However, in the southern coast the average rainfall is 300 millimeters.
Owing to the influence of the Andes, Chile's annual rainfall varies immensely since the winds in the north are the reverse direction from those in the south.
In the north, there is literally no rainfall owing to the powerful upwelling created by the subtropical high and the Peruvian Upwelling, which creates a temperature inversion and suppresses precipitation enough to allow 6,700 metre high Llullaillaco to be the highest glacier-free mountain in the world.
Between 27˚S and 40˚S, rainfall in Chile increases steadily from around 50 millimetres (2 inches) to 2,000 millimetres (80 inches). This rainfall is concentrated in a rainy season ranging in length from two months (June, July) in the Norte Chico to seven months (April to October) in Concepción. Annual rainfall may vary greatly, being typically highest in El Niño years: for instance in Santiago annual rainfall has ranged from 825.7 millimetres (32.5 inches) in 1900 to 66.1 millimetres (2.6 inches) in 1924. Owing to the expansion of the Hadley circulation from increased levels of CO2, CH4 and N2O, rainfall over the central part of Chile has declined by up to 40 percent since the late 1960s.
Southern Chile is in the westerly wind belt ("Furious Fifties") year-round, and is always cool and very wet except for some rain shadow areas (e.g. Chile Chico, Punta Arenas) which may have as little rainfall as Santiago. Coastal areas of southern Chile may have as much as 5,000 to 6,000 millimetres (197 to 236 inches) of rainfall, which on the higher mountains translates to 50 to 60 metres (1,970 to 2,362 inches) of snow. As a result, tidewater glaciers exist as far north as 46˚S.
Owing to the influence of the Andes, Chile's annual rainfall varies immensely since the winds in the north are the reverse direction from those in the south.
In the north, there is literally no rainfall owing to the powerful upwelling created by the subtropical high and the Peruvian Upwelling, which creates a temperature inversion and suppresses precipitation enough to allow 6,700 metre high Llullaillaco to be the highest glacier-free mountain in the world.
Between 27˚S and 40˚S, rainfall in Chile increases steadily from around 50 millimetres (2 inches) to 2,000 millimetres (80 inches). This rainfall is concentrated in a rainy season ranging in length from two months (June, July) in the Norte Chico to seven months (April to October) in Concepción. Annual rainfall may vary greatly, being typically highest in El Niño years: for instance in Santiago annual rainfall has ranged from 825.7 millimetres (32.5 inches) in 1900 to 66.1 millimetres (2.6 inches) in 1924. Owing to the poleward expansion of the descending limb Hadley circulation via increased levels of CO2, CH4 and N2O, rainfall over the central part of Chile has declined by up to 40 percent since the late 1960s.
Southern Chile is in the westerly wind belt ("Furious Fifties") year-round, and is always cool and very wet except for some rain shadow areas (e.g. Chile Chico, Punta Arenas) which may have as little rainfall as Santiago. Coastal areas of southern Chile may have as much as 5,000 to 6,000 millimetres (197 to 236 inches) of rainfall, which on the higher mountains translates to 50 to 60 metres (1,970 to 2,362 inches) of snow. As a result, tidewater glaciers exist as far north as 46˚S, whereas in the northern hemisphere the most equatorward tidewater glaciers are at 56˚N in Alaska.
The southern coast of Chile is one of the wettest places on Earth, and probably has the highest proportion of wet days of any place on Earth owing to the violent, circum-Antarctic "Furious Fifties", which hit the Andes and drench the region almost continuously.
In the wettest parts of the coast around Puerto Eden and Bahia Felix, the average annual rainfall is between 5,000 and 6,000 millimetres (200 to 240 inches). It falls on all but two days per month, year round, and consecutive dry days are exceptionally rare.
The average annual rainfall in Washington, D.C. is around 40 inches.
The average annual rainfall in Zagreb is around 33 inches.
The average rainfall is 51 inches every year . Which is 110 days a year.
For the period 1971 to 2000, the average annual rainfall in the Leicester area was approximately 700 mm
The average annual rainfall in Iran varies depending on the region. In general, Iran has a arid or semi-arid climate with average annual rainfall ranging from less than 100 mm in desert areas to around 1,000 mm in the Caspian region.
Quito is the capital of Ecuador and has an average annual rainfall of 38 inches. It is the highest official capital city in the world at an elevation of 9,350 feet.
Ecuador is a tropical rainfall because it has the equator going through it.
The average annual rainfall in Washington, D.C. is around 40 inches.
The average annual rainfall in Zagreb is around 33 inches.
the average rainfall in Indonesia is 133 mm
Nevada's average rainfall is 9 inches
what is the yearly average rainfall of spain?
The average rainfall for Olympia is 50 inches a year.
What is the average rainfall for the year in an ocean ecosystem?
The average rainfall is 51.3 inches.
What is the average yearly rainfall in Hong Kong?
Romania's average yearly rainfall is 670 mm.