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Get the Rawalpindi, Punjab local weather forecast by the hour and the next 10 days. Skip to main content. Sign in. Mail. 24/7 Help. For premium support please call: 800-290-4726 more ways ...
Climate of Rawalpindi. Coordinates: 33.6°N 73.05°E. Rawalpindi features a humid subtropical climate ( Köppen: Cwa) with hot summers, and cool to cold winters. Its climate is classified as very similar to its twin city Islamabad, but the geographical location and extreme urbanization of Rawalpindi has led to weather and climatic conditions ...
Rawalpindi (/ rɔːlˈpɪndi /; Punjabi, Urdu: راولپنڈی, romanized:Rāwalpinḍī; pronounced [ɾɑːʋəlpɪnɖiː] ⓘ [ 5 ]), colloquially known as Pindi, is the third-largest city in the Pakistani province of Punjab. It is a commercial and metropolitan city, being the fourth most populous in Pakistan. It is located near the Soan ...
Larkana. Sindh. It was the highest recorded temperature in Pakistan in 2016. 50 °C (122 °F) or above was recorded for four consecutive days from 17 to 20 May 2016. [11] 30 May 2009. 52 °C (126 °F) Turbat. Balouchistan. 50 °C (122 °F) or above was recorded for five consecutive days from 26 to 29 May 2009.
Climate of Islamabad. The climate of Islamabad is a humid subtropical climate (Köppen climate classification) with four seasons: a pleasant Spring (March–April), a hot Summer (May–August), a warm dry Autumn (September—October), and a cold Winter (November—February). The hottest month is June, where average highs routinely exceed 37 °C ...
Website. pmd.gov.pk. The Pakistan Meteorological Department (PMD) (Urdu: محکمہ موسمیات پاکستان, also known as Pakistan Met Office[3][4]), is an autonomous and independent institution tasked with providing weather forecasts and public warnings concerning weather for protection, safety and general information. [1]
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 ...
There was a gradually accentuating upper air westerly trough at 500 hpa between 40-50ºN and 60-70ºE and there were strong monsoon incursions from the Arabian Sea and the Bay of Bengal while the southwesterly monsoon current from the Arabian Sea showed strong convergence over Islamabad, Rawalpindi District and Hazara and Malakand Divisions and ...
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