Incensement of Temperature Triggered to Induce Severe Drought in Thar Desert, Pakistan

S. Meghwar, G. M. Mastoi, K. F. Almani, A. G. Sahito, K. H. Lashari, M. Ali, M. Panhwar, S. Rahoojo, A. Hingorjo
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Abstract

In deserts an increase or even a small change in temperature can set ideal conditions for drought; the prolonged conditions can lead to an agricultural drought from the metrological drought. We have applied SPSS and SPI to investigate Global climate model temperature variation as a drought driven element. Met-data of two meteorological stations was analyzed to reveal the condition. The obtained results show that temperature has risen from 1oC to2.5oCin20th century. The data also demonstrates a negative correlation between temperature and drought.
温度升高引发巴基斯坦塔尔沙漠严重干旱
在沙漠中,温度的升高甚至是微小的变化都可能为干旱创造理想的条件;长期的气候条件会导致农业干旱,而不是气象干旱。我们应用SPSS和SPI对全球气候模式温度变化作为干旱驱动因素进行了研究。分析了两个气象站的气象资料,揭示了这一情况。结果表明,20世纪气温已从10℃上升到2.5℃。数据还表明温度和干旱之间呈负相关。
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