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The irregularity in the amount of rainfall in different parts of the north Indian plains is mainly due to
Irregularity intensity of low pressure in the north-western parts of India
Variation in the location of the axis of low pressure through
Difference in frequency of cyclones
Variation in the amount of moisture
During the Monsoon season, there are periods when the Monsoon trough shifts to the foothills of Himalayas, which leads to sharp decrease in rainfall over most parts of the country but increase along the Himalayas and parts of Northeast India and Southern Peninsula.
During July and August, there are certain periods when the monsoons become weak. Rainfall practically ceases over the country outside the Himalayan belt and southeast peninsula. This is known as break in the monsoon.
Breaks are likely to occur during the second week of August and last for a week. The breaks are believed to be brought about by the northward shifting of the monsoon trough (minimum low pressure cell in ITCZ). The axis of the trough lies at the foothills of the Himalayas during the break period.
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