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Arid

Index Arid

A region is arid when it is characterized by a severe lack of available water, to the extent of hindering or preventing the growth and development of plant and animal life. [1]

20 relations: Africa, Arid Diagonal, Arid Forest Research Institute, Aridification, Aridity index, Atmosphere, Australia, Central America, Climate change, Desert, Desert climate, Deserts and xeric shrublands, Desiccation tolerance, Drought, Equator, Erikson's stages of psychosocial development, Morphogenesis, Relative humidity, Semi-arid climate, Vapor pressure.

Africa

Africa is the world's second largest and second most-populous continent (behind Asia in both categories).

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Arid Diagonal

BWk climate running from Ecuador to Southern Patagonia. The Arid Diagonal (diagonal árida/arreica) is a contiguous zone of arid and semi-arid climate that traverses South America from coastal Peru in the Northwest to Argentine Patagonia in Southeast including large swathes of Bolivia and Chile.

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Arid Forest Research Institute

Arid Forest Research Institute (AFRI) is a research institute situated in Jodhpur, Rajasthan, India.

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Aridification

Aridification is the process of a region becoming increasingly dry.

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Aridity index

An aridity index (AI) is a numerical indicator of the degree of dryness of the climate at a given location.

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Atmosphere

An atmosphere is a layer or a set of layers of gases surrounding a planet or other material body, that is held in place by the gravity of that body.

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Australia

Australia, officially the Commonwealth of Australia, is a sovereign country comprising the mainland of the Australian continent, the island of Tasmania and numerous smaller islands.

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Central America

Central America (América Central, Centroamérica) is the southernmost, isthmian portion of the North American continent, which connects with the South American continent on the southeast.

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Climate change

Climate change is a change in the statistical distribution of weather patterns when that change lasts for an extended period of time (i.e., decades to millions of years).

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Desert

A desert is a barren area of landscape where little precipitation occurs and consequently living conditions are hostile for plant and animal life.

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Desert climate

The Desert climate (in the Köppen climate classification BWh and BWk, sometimes also BWn), also known as an arid climate, is a climate in which precipitation is too low to sustain any vegetation at all, or at most a very scanty shrub, and does not meet the criteria to be classified as a polar climate.

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Deserts and xeric shrublands

Deserts and xeric shrublands are a biome characterized by receiving only a small amount of moisture, usually defined as less than 250 mm of annual precipitation.

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Desiccation tolerance

Desiccation tolerance refers to the ability of an organism to withstand or endure extreme dryness, or drought-like conditions.

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Drought

A drought is a period of below-average precipitation in a given region, resulting in prolonged shortages in the water supply, whether atmospheric, surface water or ground water.

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Equator

An equator of a rotating spheroid (such as a planet) is its zeroth circle of latitude (parallel).

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Erikson's stages of psychosocial development

Erikson's stages of psychosocial development, as articulated in the second half of the 20th century by Erik Erikson, in collaboration with Joan Erikson, is a comprehensive psychoanalytic theory that identifies a series of eight stages, in which a healthy developing individual should pass through from infancy to late adulthood.

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Morphogenesis

Morphogenesis (from the Greek morphê shape and genesis creation, literally, "beginning of the shape") is the biological process that causes an organism to develop its shape.

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Relative humidity

Relative humidity (RH) is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at a given temperature.

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Semi-arid climate

A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not as low as a desert climate.

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Vapor pressure

Vapor pressure or equilibrium vapor pressure is defined as the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system.

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Redirects here:

Arid region, Aridity, Aridness, Dry climate, Dry weather, Hyper-arid.

References

[1] https://en.wikipedia.org/wiki/Arid

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