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Loo (wind)

Hot, summer wind

  • 3 min read
  • 4 chapters

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Through Wind, Indo-Gangetic Plain and Pakistan

Since it causes extremely low humidity and high temperatures, the Loo also has a severe drying effect on vegetation leading to widespread browning in the areas affected by it during the months of May and June.

Origin and ending

The Loo mainly originates in the large desert regions of the northwestern parts in the indian subcontinent: the Great Indian Desert, the Cholistan Desert and the desert areas of Southern Balochistan.

The Loo ends in late summer, with the arrival of the Indian monsoon. In some areas of North India and Pakistan, there are brief but violent dust storms known as Kali Andhi (or black Storm) before the monsoon sets in. The arrival of monsoon clouds in any location is frequently accompanied with cloudbursts, and the sudden transformation of the landscape from brown to green can seem "astonishing" as a result of the ongoing deluge and the abrupt cessation of the Loo.

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