Abstract

The research covenants amid the evaluation and analysis of the weather data in regards to mean monthlytemperature, precipitation, rainy days, relative humidity, wind direction, atmospheric pressure, evaporation, solarradiation and with the literature cited. The components getting fluctuation in the atmospheric condition comprise ofglobal location, vicinity to ocean, geomorphic reliefs and continental extent, maritime affects, forests and landuse.Based on the daily and monthly temperature, the study area has divided into five localities consisting of hot, warm,mild, cool, and cold. Besides, the five precipitation zones namely arid, semi-arid, sub-humid, humid andundifferentiated highlands have been distinguished during course of work. Generally, eastern longitudes of the countryget substantial downpours amid summers (monsoon season). Though the western areas in winters excluding GilgitBaltistan, where it is from local thunderstorms. Pakistan encounters four precipitation seasons namely winter, premonsoon, monsoon, and post monsoon rainfall. Because of sub-tropical vicinity, the country has experienced twofundamental seasons explicitly winter and summer. Generally, the summer period goes on for five months in mountainsand seven months in plains, whilst the winter period differs for seven months in mountains and five months in plains.The stated two essential rainy periods are auxiliary sub-isolated into four sub-spells to be precisely hot, warm, monsoonand cold season. Based on appropriation and fluctuation of climate variables, Pakistan is classified in five macro areasthat auxiliary sub-curved up into 18 meso and 46 micro scale climate regions.

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