autocorrelated disturbances - meaning and definition. What is autocorrelated disturbances
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What (who) is autocorrelated disturbances - definition

WESTERN DISTURBANCE OVER NORTH INDIA
Western disturbances; Western disturbance
  • A strong western disturbance affecting the northern parts of the Indian subcontinent in February 2013. Such disturbances bring substantial amount of rainfall and are a threat to lives and property.
  • A western disturbance moving east towards the Indian subcontinent. It can be seen as a cloud patch originating from the [[Black Sea]], progressing east thereafter.
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Bangalore disturbances         
RIOTS IN BANGALURU IN 1928
Bangalore Disturbances 1928; Bangalore disturbances 1928; Bangalore Disturbances
The Bangalore disturbances of 1928, also known as Ganapati Galabhe and Hindu-Muslim Gharshane, were a series of Hindu-Muslim clashes which took place in the city of Bengaluru in June – July 1928 over construction of a niche on a Ganesha idol in a school premises. These were the first major communal disturbances of Bengaluru.
Anahuac disturbances         
UPRISINGS OF SETTLERS IN TEXAS IN 1832 AND 1835
Anahuac Disturbance; Battle of Anahuac; Anahuac Disturbances
The Anahuac disturbances were uprisings of settlers in and around Anahuac, Texas, in 1832 and 1835 which helped to precipitate the Texas Revolution. This eventually led to the territory's secession from Mexico and the founding of the Republic of Texas.
Punjab Disturbances Court of Inquiry         
Punjab Disturbances Court Of Inquiry
On 19 June 1953 a Court of Inquiry was established to look into disturbances in the Punjab, Pakistan caused by agitation against the Ahmadiyya minority group. The disturbances prompted Martial law to be declared and dozens were killed by the military in the process of their quelling.

Wikipedia

Western Disturbance

A western disturbance is an extratropical storm originating in the Mediterranean region that brings sudden winter rain to the northern parts of the Indian subcontinent, which extends as east as up to northern parts of Bangladesh and South eastern Nepal. It is a non-monsoonal precipitation pattern driven by the westerlies. The moisture in these storms usually originates over the Mediterranean Sea, the Caspian Sea and the Black Sea. Extratropical storms are a global phenomena with moisture usually carried in the upper atmosphere, unlike their tropical counterparts where the moisture is carried in the lower atmosphere. In the case of the Indian subcontinent, moisture is sometimes shed as rain when the storm system encounters the Himalayas. Western disturbances are more frequent and stronger in the winter season.

Western disturbances are important for the development of the Rabi crop , which includes the locally important staple wheat.