Seterra
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  • Arabistan Çölü
  • Atacama Çölü
  • Black Rock Çölü
  • Büyük Kumlu Çöl
  • Büyük Victoria Çölü
  • Chihuahuan Çölü
  • Gobi Çölü
  • Kalahari Çölü
  • Karakum Çölü
  • Mojave Çölü
  • Namib Çölü
  • Necef Çölü
  • Patagonya Çölü
  • Sahra Çölü
  • Simpson Çölü
  • Sina Çölü
  • Sonora Çölü
  • Suriye Çölü
  • Tabernas Çölü
  • Taklamakan Çölü
  • Tar Çölü
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Deserts primarily occur in two bands of latitude in the world. Moving both north and south from the equator, tropical air containing moisture slowly cools and drops its water in the form of rain. As the air continues to move away from the equator most of its moisture has already been dropped, and there is virtually nothing left by the time it reaches the location of the world’s deserts. Some places that would otherwise be a desert receive rain from the jet stream that transports moisture from the ocean.

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