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Characterization of drought using four drought indices under climate change in the Sahel region of Nigeria: 1981-2015

机译:尼日利亚Sahel地区气候变化下四次干旱指数的干旱特点:1981-2015

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Drought is a natural hazard that has affected agriculture which is the main livelihood of the people in the Sahel region of Nigeria (SRN) in the last few decades. Continental and regional drought monitoring is very essential for the development of an early warning system especially in the context of global warming. The severity of drought was simulated to evaluate climate change impacts on drought conditions in the SRN using the standardized precipitation evapotranspiration index (SPEI), the standardized precipitation index (SPI), the original and self-calibrated Palmer drought severity indices (PDSI and scPDSI). The difference between the Hargreaves (Har) and Penman-Monteith (PM) potential evapotranspiration (PET) models used for the computation of the SPEI were also studied. The Mann-Kendall test was used to analyze the trends and significance of the climatic data. The time series of four drought indices were compared at six synoptic stations within the SRN. The influences of climate change on drought conditions were examined with a hypothetical gradual precipitation changes (+ 10%) and 2 degrees C increase in temperature. The findings showed that there was a significant correlation between Har and PM models, and between the SPEIs estimated from the two PET models. However, a major drought episode (1982-1983) indicated by SPEI-PM was not captured under SPEI-Har. Considering climate change conditions, the severity and intensity of drought increases as the twenty-first century progresses under both the scPDSI and SPEI mainly due to more demand for moisture based on a temperature rise of 2 degrees C. Either a slight (10%) increase or decrease in the monthly accumulation of rainfall depth will not have a significant impact on drought, if there is a slight increase in temperature as it is being currently observed in the SRN. Thus, it is pertinent for stakeholders to critically consider establishing policies that can ameliorate this phenomenon as the twenty-first century progresses.
机译:干旱是一种自然危害,受到影响的农业,这是尼日利亚萨赫勒地区(SRN)的主要生计在过去的几十年中。欧式和区域干旱监测对于开发早期预警系统的发展是至关重要的,特别是在全球变暖的背景下。模拟干旱的严重程度,以评估使用标准化降水蒸发指数(SPEI),标准化降水指数(SPI),原始和自我校准的Palmer干旱严重指数(PDSI和SCPDSI)的气候变化对SRN中干旱状况的影响。还研究了Hargreaves(Har)和Penman-Monteith(PM)电位蒸散(PET)模型的差异,用于计算Spei的计算。 Mann-Kendall测试用于分析气候数据的趋势和意义。在SRN内的六个舞台上比较了四个干旱指标的时间序列。检查气候变化对干旱条件的影响,并在假设的逐渐降水变化(+ 10%)和2℃的温度上增加。结果表明,HAR和PM模型之间存在显着的相关性,以及从两种PET模型估计的SPEI之间。然而,Spei-Har未捕获Spei-PM所示的主要干旱集团(1982-1983)。考虑到气候变化条件,随着250世纪的二十一世纪的进展,干旱的严重程度和强度主要是由于基于2摄氏度的温度升高的水分需求更多。轻微(10%)增加或者降雨量的每月积累的减少对干旱不会产生重大影响,如果温度略有增加,因为当前在SRN中观察到。因此,对于利益相关者来说,批评者认为建立可以改善这种现象的政策,这是二十一十世纪的进展。

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