温度升高引发巴基斯坦塔尔沙漠严重干旱

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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引用次数: 0

摘要

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。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Incensement of Temperature Triggered to Induce Severe Drought in Thar Desert, Pakistan
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.
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