2001 Islamabad cloud burst
Causes
The cloud burst was the result of the sequel of vigorously developed cloud due to the combined effect of well marked westerly trough (Westerly wave), passing over 500hpa with enough supply of moisture from southwest monsoon.

2001 Islamabad cloud burst

Section Title: Causes
Table Section Text: The cloud burst was the result of the sequel of vigorously developed cloud due to the combined effect of well marked westerly trough (Westerly wave), passing over 500hpa with enough supply of moisture from southwest monsoon.

Name of Station	Location	0500–0800 PST	0800–1100 PST	1100–1400 PST	1400–1700 PST	Total Rainfall from 0500 to 1700 PST

PMD Headquarters	Islamabad	42 millimetres (1.7 in)	132 millimetres (5.2 in)	400 millimetres (16 in)	46 millimetres (1.8 in)	620 millimetres (24 in)

Saidpur	Islamabad	103 millimetres (4.1 in)	Did not measure	Did not measure	314 millimetres (12.4 in)	417 millimetres (16.4 in)

Shamsabad	Rawalpindi	04 millimetres (0.16 in)	83 millimetres (3.3 in)	200 millimetres (7.9 in)	48 millimetres (1.9 in)	335 millimetres (13.2 in)

Airport	Rawalpindi	Traces	06 millimetres (0.24 in)	65 millimetres (2.6 in)	99 millimetres (3.9 in)	170 millimetres (6.7 in)

Sentence(s)

Rawalpindi experienced 335 millimetres (13.2 in) of rain during the 2001 Islamabad cloud burst.

final_sentence: Rawalpindi experienced 335 millimetres (13.2 in) of rain during the 2001 Islamabad cloud burst.