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Every month in Rawalpindi is marked by its own unique characteristics, conditions and weather pattern. Following is also a summary of each month's averages and records. January. January is the coldest month in Rawalpindi with an average low of 3.1 °C (37.6 °F) and a record low of −3.9 °C (25.0 °F) recorded in 1967.
Highest rainfall was recorded in Jacobabad with the record of 481 millimetres (18.9 in) in just 7 days and 441 millimetres (17.4 in) in just 36 hours. Other records are 239 millimetres (9.4 in) in Larkana while 206 millimetres (8.1 in) in Sukkur. Larkana division was worst hit by heavy rainfall.
The climate in the capital city of Islamabad varies from an average daily low of 2 °C in January to an average daily high of 38 °C in June. Half of the annual rainfall occurs in July and August, averaging about 255 millimeters in each of those two months. The remainder of the year has significantly less rain, amounting to about fifty ...
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Climate change in Pakistan is a major issue for the country. Pakistan is highly vulnerable to climate change. As with the changing climate in South Asia as a whole, the climate of Pakistan has changed over the past several decades, with significant impacts on the environment and people. [1] In addition to increased heat, drought and extreme ...
The weather is highly variable due to the proximity of the city to the foothills of Himalayas. The average annual rainfall is 1,254.8 mm (49.40 in), most of which falls in the summer monsoon season. However, westerly disturbances also bring quite significant rainfall in the winter.
The Punjabi calendar ( Punjabi: ਪੰਜਾਬੀ ਜੰਤਰੀ, پنجابی جنتری) is a luni-solar calendar used by the Punjabi people in Punjab and around the world, but varies by religions. Historically, the Punjabi Sikhs and Punjabi Hindus have used the ancient Bikrami (Vikrami) calendar. [1] [2] Punjabi Muslims use the Arabic ...
Islamabad's twin city, Rawalpindi experienced 335 millimetres (13.2 in) of rain during this event. Causes [ edit ] 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 500 hpa with enough supply of moisture from southwest monsoon .
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