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Climate Of Faisalabad
The climate of Faisalabad features a semi-arid climate (BSh) in Köppen-Geiger classification, bordering a humid subtropical climate (Cwa) with very hot and humid summers and dry cool winters. The average maximum and minimum temperatures in June are and . In January the average minimum and maximum are and .Faisalabad: it's Pakistan
The summer season starts in mid-April and continues until late October. May and June are the hottest months, while July, August and the first half of September can be oppressively humid, except for the days when it rains. June is the hottest month in Faisalabad, when conditions are dry and dust storms are common. The coldest month is January, which is also a dry month with significant foggy days. The fog is particularly dense at night and in early morning hours. The winter season starts i ...
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Faisalabad
Faisalabad (; Punjabi/ ur, , ; ), formerly known as Lyallpur (Punjabi, Urdu: لائل پور), named after the founder of the city, but was renamed in 1977 in honour of late King Faisal of Saudi Arabia. It is the 3rd largest city of Pakistan after Karachi and Lahore respectively, and the 2nd largest city of Punjab after Lahore. Faisalabad is one of Pakistan's wealthiest cities, the largest industrial hub and 2nd largest city of wider Punjab region. Historically one of the first planned cities within British India, it has long since developed into a cosmopolitan metropolis. Faisalabad was restructured into city district status; a devolution promulgated by the 2001 local government ordinance (LGO). The total area of Faisalabad District is while the area controlled by the Faisalabad Development Authority (FDA) is . Faisalabad has grown to become a major industrial and distribution centre because of its central location in the region and connecting roads, rails, and ...
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Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multip ...
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Humid Subtropical Climate
A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates. It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classification was officially created under the Trewartha climate classification. In this classification, climates are termed humid subtropical when ...
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Climate Of Lahore
Lahore features a five-season semi-arid climate (Köppen climate classification ''BSh''), closely bordering a humid subtropical climate, with five seasons: foggy winter (10 Dec – 1 Feb) with few western disturbances causing rain; pleasant spring (16 Feb – 15 April); summer (15 April – 30 June) with dust, rain storms and heat wave periods; rainy monsoon (1 July – 16 September); and dry autumn (16 September –14 November). However, in some cases, it can be classified as being humid subtropical (Cwa), rather than semi-arid, since it has well defined seasons and an ample amount of rain. It occasionally has very prolonged and dense monsoons, typical of a humid subtropical climate. The hottest month is June, where average highs routinely exceed . The wettest month is July, with heavy rainfalls and evening thunderstorms with the possibility of cloudbursts. The coolest month is January with dense fog. The city's record high temperature was , recorded on 5 June 2003. On 10 ...
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Climate Of Rawalpindi
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 that are notably different from its twin. Rawalpindi's weather has historically been known to change rather quickly due to its proximity to Himalayas and the Pir Panjal Range. These mountains not only influence the weather of the city, but also provide great recreation during the hot months. Furthermore, Its warm comfortable mean annual temperature of attracts people to live here permanently from all over Pakistan. The average annual rainfall is abundant at , most of which falls in the monsoon season. However, frontal cloud bands also bring significant rainfall in the winter. In summers, June is the hottest with record maximum temperature at a blistering recorded on 13 June 1953. On the oth ...
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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 . The wettest month is July, with heavy rainfall and evening thunderstorms with the possibility of cloudburst. The coldest month is January, with temperatures variable by location. In Islamabad, temperatures vary from cold to mild, routinely dropping below zero. In the hills there is sparse snowfall. The weather ranges from a minimum of in January to a maximum of in June. The average low is in January, while the average high is in June. The highest temperature recorded was in June, while the lowest temperature was in January. On 23 July 2001, Islamabad received a record breaking of rainfall in just 10 hours. It was the heaviest rainfall in Pakistan during the pas ...
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List Of Extreme Weather Records In Pakistan
The weather extremes in Pakistan include extremely high and extremely low temperatures, heaviest rainfalls and floodings. Pakistan has one of the highest temperature ranges in the world (temperature range refers to the difference between highest and lowest recorded temperatures ever) with proven weather conditions ranging from as high as like those in the Sahara desert, to as low as those like in Alaska making it one of the most climatically diverse countries in the world. The highest temperature ever recorded in Pakistan is which was recorded in Turbat, Balochistan on 28 May 2017. It was not only the hottest temperature ever recorded in Pakistan but also the hottest reliably measured temperature ever recorded on the continent of Asia and the fourth-highest temperature ever recorded on Earth. The second-highest temperature ever recorded in Pakistan is which was recorded in Moenjo Daro, Sindh on 26 May 2010. It is fifth-highest temperature ever recorded on Earth. The highest ...
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Climate By City In Pakistan
Climate is the long-term weather pattern in an area, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, including the atmosphere, hydrosphere, cryosphere, lithosphere and biosphere and the interactions between them. The climate of a location is affected by its latitude/longitude, terrain, altitude, land use and nearby water bodies and their currents. Climates can be classified according to the average and typical variables, most commonly temperature and precipitation. The most widely used classification scheme was the Köppen climate classification. The Thornthwaite system, in use since 1948, incorporates evapotranspiration along with temperature and ...
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