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Changing characteristics of meteorological droughts in Nigeria during 1901-2010

机译:1901-2010年尼日利亚气象干旱的变化特征

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摘要

The objective of this study was to assess the changes in the severity and return periods of meteorological droughts during major cropping seasons of Nigeria for the period 1901-2010 in order to understand the impacts of climate variation on seasonal droughts. Gauge-based gridded global precipitation climatology center (GPCC) rainfall and climate research unit (CRU) potential evapotranspiration (PET) data having a spatial resolution of 0.5 degrees were used for the reconstruction of droughts using standardized precipitation evapotranspiration index (SPEI). SPEI values were fitted with the best distribution function to estimate seasonal droughts return periods and the modified Mann-Kendall test was used to assess the secular changes in climate variables and drought index. The temporal variations in droughts and their interrelations with rainfall and temperature trends were assessed using a 50-year moving window with a 10-year time step. The results showed that meteorological drought severity has increased for all the cropping seasons of Nigeria. Temperature was found to be the dominating factor for defining droughts in semi-arid regions in the north while rainfall in the monsoon and tropical savanna climatic zones dominates in the south. Rises in temperature in the range of 0.14-0.42 degrees C/decade and almost no change in rainfall have caused decreases in SPEI up to -0.25/decade in some regions. The number of grid points with decreasing SPEI was found to vary between 50 out of 323 for millet and 152 for yam growing season. The moderate droughts were found to become more frequent compared to other classes of droughts. Amongst the cropping seasons, the highest increases in drought frequency were observed during corn growing season. The highest decrease in the median value of the return period of moderate, severe and extreme droughts during the two corn growing seasons were observed to be 6.25, 12.86 to 13.20, 23.15 to 24.31 years in 1901-1950 to 6.25, 12.92 to 12.94, 23.51 to 23.64 in 1961-2010. Compared to other drought severities, the return periods of the moderate droughts were found to decrease more. A general decrease in the return periods of droughts indicates more frequent droughts during all cropping seasons of Nigeria. Therefore, it can be concluded that the rising temperature due to global warming would increase drought severity and frequency in all the cropping seasons of Nigeria.
机译:这项研究的目的是评估1901-2010年尼日利亚主要农作物季节气象干旱的严重程度和恢复期的变化,以便了解气候变化对季节性干旱的影响。基于尺度的网格化全球降水气候中心(GPCC)降雨和气候研究单位(CRU)的潜在蒸散量(PET)数据具有0.5度的空间分辨率,用于使用标准化的降水蒸散指数(SPEI)重建干旱。 SPEI值具有最佳的分布函数,可以估算季节性干旱的重现期,改良的Mann-Kendall检验用于评估气候变量和干旱指数的长期变化。干旱的时空变化及其与降雨和温度趋势的相互关系,是使用50年的移动窗口和10年的时间步长进行评估的。结果表明,在尼日利亚的所有种植季节,气象干旱的严重程度都有所增加。人们发现,温度是决定北部半干旱地区干旱的主要因素,而季风和热带稀树草原气候区的降雨量主要是南部。温度升高在0.14-0.42摄氏度/十年的范围内,并且几乎没有降雨变化引起SPEI下降,在某些地区最高达到-0.25 /十年。发现SPEI降低的网格点数量在小米的323个中的50个与山药生长季节的152个之间变化。与其他类别的干旱相比,中度干旱被发现更为频繁。在整个种植季节中,玉米生长季节的干旱频率增幅最大。 1901-1950年至6.25年,6.25年,12.92至12.94、23.51年,两个玉米生长季中度,重度和极端干旱的重现期中值最大降幅分别为6.25、12.86至13.20、23.15至24.31年在1961-2010年达到23.64。与其他干旱严重程度相比,中度干旱的重现期减少得更多。干旱恢复期的普遍减少表明,在尼日利亚所有种植季节,干旱更加频繁。因此,可以得出结论,由于全球变暖导致的温度升高将增加尼日利亚所有种植季节的干旱严重程度和频率。

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