Senin, 15 Mei 2017

Global Ecology



Global Air Circulation and
Precipitation Patterns

Intense solar radiation near the equator initiates a global pattern of air circulation and precipitation. High temperatures in the tropics evaporate water from Earth’s surface and cause warm, wet air masses to rise (blue arrows) and flow toward the poles. The rising air masses release much of their water content, creating abundant precipitation in tropical regions. The high-altitude air masses, now dry, descend (tan arrows) toward Earth around 30° north and south, absorbing moisture from the land and creating an arid climate conducive to the development of the deserts that are common at those latitudes. Some of the descending air then flows toward the poles. At latitudes around 60° north and south, the air masses again rise and release abundant precipitation (though less than in the tropics). Some of the cold, dry rising air then flows to the poles, where it descends and flows back toward the equator, absorbing moisture and creating the comparatively rainless and bitterly cold climates of the polar region




Figure : Air flowing close to Earth’s surface creates predictable global wind patterns. As Earth rotates on its axis, land near the equator moves faster than that at the poles, deflecting the winds from the vertical paths shown above and creating the more easterly and westerly flows shown at left. Cooling trade winds blow from east to west in the tropics; prevailing westerlies blow from west to east in the temperate zones, defined as the regions between the Tropic of Cancer and the Arctic Circle and between the Tropic of Capricorn and the Antarctic Circle.

factors—temperature, precipitation, sunlight, and wind— are particularly important components of climate. In this section, we will describe climate patterns at two scales: macroclimate, patterns on the global, regional, and landscape level; and microclimate, very fine, localized patterns, such as those encountered by the community of organisms that live in the microhabitat beneath a fallen log. 

Campbell, dkk. 2008. Biologi Jilid 3. Jakarta: Erlangga.


3 komentar:

  1. postingan yang bagus, terima kasih infonyaa

    BalasHapus
  2. info yang menarik :) thanks ditunggu postingan lainnya

    BalasHapus
  3. jadi berdasarkan tulisan saudara, dari mana asalnya angin di bumi ini? dan juga setujukah anda jika bumi ini datar?

    BalasHapus