Western Disturbances
Western Disturbances
Western Disturbances. Western Disturbance is an atmospheric system formed from temperate cyclones originating in the Mediterranean region. These storms bring sudden winter.
Rainfall in the northwestern parts of the Indian subcontinent is known as Western Disturbance. It is a global climate event.
They enter the Indian subcontinent in winter due to the southward shift of the pressure belts in the Mediterranean Sea and are responsible for the winter rainfall. They originate from the Caspian Sea. And the land is in the middle sea.
Western Disturbances | Temperate Cyclone
Western Disturbances. These cyclones are formed by meeting of warm and cold air masses at the meeting place of cold front and warm front. They move from west to east under the influence of westerly winds. They affect the weather of entire Europe.
Western Disturbances | Impact on climate
- It plays an important role in bringing moderate to heavy rain in the low-lying areas and heavy snow in the hilly regions of the Indian subcontinent.
- Their arrival is usually accompanied by cloudy skies, high night temperatures and unusual rainfall.
- The monsoon rains that result from these are extremely beneficial for rabi crops.
- They are the carriers of cold wave in the Indian Gangetic plain.
Western Disturbances | Mavath
The rain that occurs in winter due to Western Disturbance is called Maavath
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