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For the Australian television series see Rain Shadow (TV series). Rain Shadow is an Australian Television Drama series which premiered on 7 October 2007 on ABC TV. For the Australian Gothic Metal band, see Rainshadow. For a topic outline on this subject see List of basic Australia topics.

A rain shadow or rainshadow, or more accurately, precipitation shadow, is a dry region of land that is leeward of or behind a mountain, with respect to prevailing wind direction. Windward is the direction from which the wind is blowing at the time in question A mountain is a Landform that extends above the surrounding Terrain in a limited area with a peak Wind is the flow of Air or other Gases that compose an Atmosphere (including but not limited to the Earth's)

Contents

Description

A rain shadow is usually caused by a mountain range, but can be caused by other things as well, although to a much less degree. A mountain range is a chain of Mountains bordered by highlands or separated from other mountains by passes or valleys

A rainshadow is warm and dry because as moist air masses rise to the top of a mountain range or large mountain, the air cools and the moisture content decreases until it reaches the dew point, the point at which the water vapor condenses as rain, and then falls either on the windward side or atop the mountain. Water content or moisture content is the quantity of Water contained in a material such as Soil (called soil moisture) rock, The dew point (sometimes spelled dewpoint) is the Temperature to which a given parcel of Air must be cooled at constant Barometric pressure, General properties of water vapor Evaporation/sublimation Whenever a water molecule leaves a surface it is said to have evaporated Rain is Liquid precipitation. On Earth it is the condensation of atmospheric Water vapor into drops heavy enough to fall often making it to Windward is the direction from which the wind is blowing at the time in question This is called orographic lift precipitation. Orographic lift occurs when an Air mass is forced from a low Elevation to a higher elevation as it moves over rising terrain In Meteorology, precipitation (also known as one class of hydrometeors, which are atmospheric water phenomena is any product of the condensation of atmospheric The effect of this phenomenon is the creation of an arid region on the leeward side of the mountains. In general terms the Climate of a local or region is said to be arid when it is characterized by a severe lack of available Water, to the extent of hindering Also, the warm air absorbs moisture from the already dry and warm air (see Foehn winds). A foehn wind or föhn wind is a type of dry downslope wind which occurs in the lee of a mountain range The land gets little precipitation because all the moisture is lost on the mountains. Furthermore, the warm air absorbs moisture from the already dry land. [1]

Regions of notable rain shadow

There are regular patterns of prevailing winds found in bands round the Earth's equatorial region. The prevailing winds are the trends in speed and direction of Wind over a particular point on the Earth 's surface The equator (sometimes referred to colloquially as "the Line") is the intersection of the Earth 's surface with the plane perpendicular to the The zone designated the trade winds is the zone between about 30° N. The trade winds (also called trades) are the prevailing pattern of easterly winds found in the Tropics near the Earth's Equator. and 30° S. , blowing predominantly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere. Northern Hemisphere is the half of a Planet that is North of the Equator —the word hemisphere literally means 'half ball' Southern Hemisphere is the half of a Planet that is South of the Equator —the word hemisphere literally means 'half ball' The westerlies are the prevailing winds in the middle latitudes between 30 and 60 degrees latitude, blowing predominantly from the southwest in the Northern Hemisphere and from the northwest in the Southern Hemisphere. The Westerlies or the Prevailing Westerlies are the prevailing winds in the Middle latitudes between 30 and 60 degrees Latitude, blowing from The middle latitudes are between 33 degrees 33' 33" North and 66 degrees 33' 33" and 64 degrees 33' 33" South and 33 degrees 33' 33" South Latitude, or Latitude, usually denoted symbolically by the Greek letter phi ( Φ) gives the location of a place on Earth (or other planetary body north or south of the The strongest westerly winds in the middle latitudes can come in the Roaring Forties between 40 and 50 degrees latitude. The Roaring Forties is a name given especially by sailors to the latitudes between 40°S and 50°S so called because of the boisterous and prevailing westerly winds

Examples of notable rain shadowing include:

Asia

South America

North America

Most rainshadows in the western United States are due to mountain ranges, notably the Sierra Nevada and Cascades,[2] that intercept rain and snowfall that would otherwise reach a valley in the lee of the mid-latitude prevailing westerlies. The United States of America —commonly referred to as the The Sierra Nevada ( Spanish for "Snowy Range" is a Mountain range located in the U

Europe

Africa

Oceania

See also

References

  1. ^ a b Whiteman, C. A foehn wind or föhn wind is a type of dry downslope wind which occurs in the lee of a mountain range David (2000). Mountain Meteorology: Fundamentals and Applications. Oxford University Press. ISBN 0-19-513271-8.  
  2. ^ USA Today. USA TODAY is a national American daily Newspaper published by the Gannett Company. How mountains influence rainfall patterns. Retrieved on 2008-02-29. 2008 ( MMVIII) is the current year in accordance with the Gregorian calendar, a Leap year that started on Tuesday of the Common Leap years Although the modern calendar counts a year as 365 days a complete revolution around the sun takes approximately 365 days and 6 hours

External links

Dictionary

rain shadow

-noun

  1. (meteorology) an area of diminished precipitation on the lee side of mountains
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