The irregularity in the amount of rain in different parts of the north Indian plains, during different years, is mainly due to the 

(a) irregular intensity of low pressure in the northwestern part of India 

(b) difference in frequency of cyclones 

(c) variations in the location of the axis of the low pressure trough 

(d) the amount of moisture carried by the winds not being the same every year


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(a) irregular intensity of low pressure in the northwestern part of India 

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