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The Holdridge life zones system is a global bioclimatic scheme for the classification of land areas. It was first published by Leslie Holdridge in 1947, and updated in 1967. It is a relatively simple system based on few empirical data, giving objective criteria. [ 1 ]
Holdridge life zone classification scheme. Although conceived as three-dimensional by its originator, is usually shown as a two-dimensional array of hexagons in a triangular frame. In 1947, Leslie Holdridge published a life zone classification using indicators of: mean annual biotemperature (logarithmic) annual precipitation (logarithmic)
Holdridge Life Zone Classification scheme. Potential evapotranspiration is the amount of evaporation that would occur if water were not limited. Annual precipitation is rain or snow. v2: Larger numbers & labels v3: Larger belts/region labels too Reason Really well illustrates Holdridge's life zones, and is visually pleasing. Articles this image ...
(The term aseasonal refers to the lack in the tropical zone of large differences in daylight hours and mean monthly (or daily) temperature throughout the year. Annual cyclic changes occur in the tropics, but not as predictably as those in the temperate zone, albeit unrelated to temperature, but to water availability whether as rain, mist, soil ...
English: Holdridge Life Zone Classification scheme. Potential evapotranspiration is the amount of evaporation that would occur if water were not limited. Annual ...
Tropical and subtropical moist forests (TSMF) as shown within the Holdridge Life Zones classification scheme, and includes moist forests, wet forests, and rainforests.
Los Angeles and other areas in California are among the highest-risk areas for wildfires — but they're not the only ones. Many fires take place in areas where humans have overstepped into nature ...
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.