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Name - Mahadev Walmik Shewale
             Class - S Y B.com
              Division - A
             Roll No.- 131525
        Project - Desert Ecosystem
Desert
 
1.1 Classification
                          
 Deserts are part of a wide classification of regions
  that, on an average annual basis, have a moisture
  deficit (for example, they lose more moisture than
  they receive)
2 Desert features
                  
   Mountain and basin deserts
   Hamada deserts, which consist of plateau landforms
   Regs, which consist of rock pavements
   Ergs, which are formed by sand seas
   Intermontane Basins
2.1 Flora
                                     
Deserts have a reputation for supporting very little life, but in reality deserts
often have high biodiversity. Some desert flora include shrubs, Prickly
Pears,Desert Holly, and the Brittlebush
Fauna
                               
Desert fauna include animals that remain hidden during daylight
hours to control body temperature or to limit moisture needs. Some
fauna includes the kangaroo rat, coyote, jack rabbit, and many lizards
Water
  dangerous.                   
  Water can quickly fill after heavy rains, and flash floodsmake these channels

The formation of the subtropical high-pressure cell.
The rain shadow effect in the belt of easterly trade winds.
The effect of the cold currents off the west coast of the continents at these
latitudes.
The depositing sands of a desert along its border into the fertile land


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Mahadev desert presentation1

  • 1. Name - Mahadev Walmik Shewale Class - S Y B.com Division - A Roll No.- 131525 Project - Desert Ecosystem
  • 3. 1.1 Classification   Deserts are part of a wide classification of regions that, on an average annual basis, have a moisture deficit (for example, they lose more moisture than they receive)
  • 4. 2 Desert features   Mountain and basin deserts  Hamada deserts, which consist of plateau landforms  Regs, which consist of rock pavements  Ergs, which are formed by sand seas  Intermontane Basins
  • 5. 2.1 Flora  Deserts have a reputation for supporting very little life, but in reality deserts often have high biodiversity. Some desert flora include shrubs, Prickly Pears,Desert Holly, and the Brittlebush
  • 6. Fauna  Desert fauna include animals that remain hidden during daylight hours to control body temperature or to limit moisture needs. Some fauna includes the kangaroo rat, coyote, jack rabbit, and many lizards
  • 7. Water dangerous.  Water can quickly fill after heavy rains, and flash floodsmake these channels The formation of the subtropical high-pressure cell. The rain shadow effect in the belt of easterly trade winds. The effect of the cold currents off the west coast of the continents at these latitudes. The depositing sands of a desert along its border into the fertile land
  • 8.

Editor's Notes

  • #7: Desert fauna include animals that remain hidden during daylight hours to control body temperature or to limit moisture needs. Some fauna includes the kangaroo rat, coyote, jack rabbit, and many lizards. These animals adapted to live in deserts are called xerocoles. Many desert animals (and plants) show especially clear evolutionary adaptations for water conservation or heat tolerance, and so are often studied in comparative physiology, ecophysiology, and evolutionary physiology. One well-studied example is the specializations of mammalian kidneys shown by desert-inhabiting species.[12] Many examples of convergent evolution have been identified in desert organisms, including between cacti and Euphorbia, kangaroo rats and jerboas, Phrynosoma and Moloch lizards. The sand cat is one of the animals that inhabits certain deserts.
  • #8: Atacama is the driest place on Earth and is virtually sterile because it is blocked from moisture on both sides by the Andes mountains and by the Chilean Coast Range. The cold Humboldt Current and the anticyclone of the Pacific are essential to keep the dry climate of the Atacama. The average rainfall in the Chilean region of Antofagasta is just 1 mm per year. Some weather stations in the Atacama have never received rain. Evidence suggests that the Atacama may not have had any significant rainfall from 1570 to 1971. It is so arid that mountains that reach as high as 6,885 meters (22,590 feet) are completely free of glaciers and, in the southern part from 25°S to 27°S, may have been glacier-free throughout the Quaternary, though permafrost extends down to an altitude of 4,400 meters and is continuous above 5,600 meters.