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Climate Variability and Drought in the Past 30 Years in Central Rift Valley of Ethiopia

机译:埃塞俄比亚中部裂谷近30年的气候变化和干旱

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The study carried out in order to analyze climate variability and drought in Rift Valley of Ethiopia. Hence, a number of analyses, such as: the Precipitation Concentration Index (PCI) and Coefficient of Variation (CV) methods are used for rainfall variability, Markov chain second order method were used in order to analysis dry spell length, while standardized rainfall anomaly were used for drought severity class. From the analysis the annual rainfall was less variable for all stations; while the seasonal variability was higher as computed using both PCI and CV methods. When the main rainy season variability was compared with the second rainy season “ Belg ”, the second rainy season was more variable for all stations. As a result, PCI value showed that Belg rainfall varied from moderate concentration to high concentration. By using INSTAT software, the historical onset and cessation date and characteristics of dry spells were investigated. It is understood that the main rainy season starts on the 174th day of the year and stops on the early second decade of September. But the variability of onset rainfall is high it may lag up to 1 month while cession data is not exceed 15 days for all stations. The 5 day probability of dry spell in the area is more than 75% even during rainy season, while 30 day dry spell is not exceed 50% even during dry season. Most of the drought years were associated for each station; even if for some station the occurrence of drought year varies by one year. But 1965, 1972-73, 1978, 1980, 1984, 1994, 1995, 2001-02, 2009 and 2014/15 show that almost all station indict there was drought index in the study area even though the drought severity degree was different. The drought frequency and intensity in central rift valley of Ethiopia is increasing trend, among 31 severe droughts 21 of them happened before 1980.
机译:进行这项研究是为了分析埃塞俄比亚裂谷的气候变化和干旱。因此,进行了许多分析,例如:降水集中指数(PCI)和变异系数(CV)方法用于降雨变异性,马尔可夫链二阶方法用于分析干旱期长度,而标准化降雨异常被用于干旱严重程度等级。根据分析,所有站的年降雨量变化较小。而使用PCI和CV方法计算得出的季节变异性更高。将主要雨季的变异性与第二个雨季“ Belg”进行比较,所有站的第二个雨季的变异性更大。结果,PCI值表明比利时的降雨量从中等浓度到高浓度变化。通过使用INSTAT软件,调查了干法的历史起止日期和特征。据了解,主要的雨季始于每年的第174天,并于9月的第二个十年初停止。但是开始降雨的变异性很高,可能会滞后1个月,而所有站点的割让数据都不会超过15天。即使在雨季,该地区5天干旱的概率也超过75%,而即使在干旱季节,30天干旱的概率也不超过50%。每个站都与大部分干旱年份相关;即使对于某些气象站,干旱年份的发生时间一年也不同。但是1965年,1972年至73年,1978年,1980年,1984年,1994年,1995年,2001-02年,2009年和2014/15年表明,即使干旱严重程度不同,几乎所有台站都指示研究区域存在干旱指数。埃塞俄比亚中部裂谷干旱频率和强度呈上升趋势,其中31次严重干旱发生在1980年之前。

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