Biome

A biome (/ˈbaɪ.oʊm/) is a distinct geographical region with specific climate, vegetation, and animal life.

[5] In the Brazilian literature, the term biome is sometimes used as a synonym of biogeographic province, an area based on species composition (the term floristic province being used when plant species are considered), or also as synonym of the "morphoclimatic and phytogeographical domain" of Ab'Sáber, a geographic space with subcontinental dimensions, with the predominance of similar geomorphologic and climatic characteristics, and of a certain vegetation form.

[6][7][8] To divide the world into a few ecological zones is difficult, notably because of the small-scale variations that exist everywhere on earth and because of the gradual changeover from one biome to the other.

[9] A 1978 study on North American grasslands[10] found a positive logistic correlation between evapotranspiration in mm/yr and above-ground net primary production in g/m2/yr.

The general results from the study were that precipitation and water use led to above-ground primary production, while solar irradiation and temperature lead to below-ground primary production (roots), and temperature and water lead to cool and warm season growth habit.

[15] Whittaker used what he called "gradient analysis" of ecocline patterns to relate communities to climate on a worldwide scale.

The multi-authored series Ecosystems of the World, edited by David W. Goodall, provides a comprehensive coverage of the major "ecosystem types or biomes" on Earth:[17] The eponymously named Heinrich Walter classification scheme considers the seasonality of temperature and precipitation.

The boundaries of each biome correlate to the conditions of moisture and cold stress that are strong determinants of plant form, and therefore the vegetation that defines the region.

A team of biologists convened by the World Wildlife Fund (WWF) developed a scheme that divided the world's land area into biogeographic realms (called "ecozones" in a BBC scheme), and these into ecoregions (Olson & Dinerstein, 1998, etc.).

As a result, vegetation forms predicted by conventional biome systems can no longer be observed across much of Earth's land surface as they have been replaced by crops and rangelands or cities.

[43][44] With its annual average temperature continuing to increase, the moisture currently located in forest biomes will dry up.

One way of mapping terrestrial biomes around the world (except the Antarctic Tundra)
Holdridge life zone classification scheme. Although conceived as three-dimensional by its originator, it is usually shown as a two-dimensional array of hexagons in a triangular frame.
The distribution of vegetation types as a function of mean annual temperature and precipitation.
Terrestrial biomes of the world according to Olson & Dinerstein et al. and used by the WWF and Global 200.
Similarities can be seen between the 14 terrestrial bioregions of Olson & Dinerstein et al. and the 17 land cover classes of the International Geosphere-Biosphere Programme , "which includes 11 natural vegetation classes, 3 developed and mosaicked land classes, and 3 non-vegetated land classes", as detected by satellites. [ 31 ]
Deciduous Needleleaf Forest
Deciduous Broadleaf Forest
Open Shrubland
Savannas
Permanent Wetlands
Urban and Built-Up
Cropland/Natural Vegetation Mosaic
Barren or Sparsely Vegetated
Predicated changes for Earth's biomes under two different climate change scenarios for 2081–2100. Top row is low emissions scenario, bottom row is high emissions scenario. Biomes are classified with Holdridge life zones system. A shift of 1 or 100% (darker colours) indicates that the region has fully moved into a completely different biome zone type. [ 46 ]