Abstract

The study discusses the climate of Balochistan with a special focus on the variation of weather conditiontaking into account the mean monthly precipitation, temperature, humidity, atmospheric circulation, air pressure,evapotranspiration and solar energy covering the time duration of 1931-2020 (normal data). The physical barriers thatbring variations in the climate of Balochistan contain geographical location, ocean, geomorphology, land use, naturalvegetation, and continental extent. Based on precipitation, the province has been divided into two main regions that arearid and semi-arid, while the temperature zones are hot, warm, mild and cool. The southern and eastern part of theprovince receives heavy rain in the summers (monsoon), whereas it is from the western depressions during the winterseason. Balochistan experiences four rainy seasons in winter (cold), pre-monsoon season (warm), monsoon season(hot), and post-monsoon season (mild). Owing to tropical (coastal) and sub-tropical continental characteristics, the areafamiliarizes two foremost seasons namely winter and summer. The summers of the area long for 5 months in hilly areaswhile 7 months in continental plains and coastal regions; whereas, winters cover five months in the plains and sevenmonths in the mountains. Based on the appropriation and fluctuation in climate constituents, Balochistan has beenclassified into two main, 6 meso, and 9 microclimate and weather zones. According to Global Climate Risk Index,2021, Pakistan has been ranked at 8th in the list of top ten global climate high-risk countries, which are exposed to theongoing climate change and requires attention to resolve the issue.

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