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首页> 外文期刊>Environment Pollution and Climate Change >Observed and Future Climate Variability, Trend and Extremes in Central Highlands of Ethiopia: A Case Study at Arsi Robe, Asasa, Debre Zeit and Kulumsa Areas
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Observed and Future Climate Variability, Trend and Extremes in Central Highlands of Ethiopia: A Case Study at Arsi Robe, Asasa, Debre Zeit and Kulumsa Areas

机译:埃塞俄比亚中部高地的观测和未来气候变化,趋势和极端事件:以Arsi Robe,Asasa,Debre Zeit和Kulumsa地区为例

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摘要

The study was conducted with the aim to analyze the variability of onset, cessation and length of growing season, and trends of daily values of temperature and precipitation extremes. The future climate data are downscaled using Marksim weather generator from the outputs of seventeen climate models (GCMs) for 2050s under RCP4.5 and RCP8.5 scenarios. The onset of the rainy season was highly variable than its cessation in the study area during the base period (1981-2015). In this regard, Asasa has experienced high variability of the onset date (CV=37%) followed by Kulumsa (CV=32.6%) and Debre Zeit (CV=32.4%) areas. The mean end of season in the study area was on 256, 298, 272 and 257 DOY at Asasa, Arsi Robe, Debre Zeit and Kulumsa sites, respectively. Analysis of 27 core set of extreme climate indices, which has been developed by ETCCDI is carried out for baseline and future periods, and the results of eighteen of them is discussed in detail in this work. The increase in lowest minimum temperature (TNn) is greater than that in highest maximum temperature (TXx) which represents the coldest or hottest days in a year, season or month respectively. The annual number of days with daily temperature greater than 25ºC referred to as summer days (SU25) will be increased highly while the frost days, when minimum temperature is less than 0ºC will be decreased in all study sites under both RCPs. Overall, the extreme temperature indices showed that, warm extremes are increasing while cold extremes decreasing in all study sites during mid-century, this series clearly indicate significant warming. From the precipitation extremes, the number of consecutive dry days (CDD) showed decreasing trend under RCP4.5 and increasing under RCP8.5 at Asasa and the reverse trend of this index is observed in Kulumsa area.
机译:进行该研究的目的是分析生长季节的发作,停止和持续时间的变异性,以及温度和极端降水的每日值的趋势。在20世纪50年代RCP4.5和RCP8.5情景下,使用Marksim气象发生器从17种气候模型(GCM)的输出中缩减了未来的气候数据。在基准时期(1981-2015年),雨季的开始与其在研究区的停止相比变化很大。在这方面,Asasa的发病日期(CV = 37%)高,其次是Kulumsa(CV = 32.6%)和Debre Zeit(CV = 32.4%)。研究区域的平均季节结束分别在Asasa,Arsi Robe,Debre Zeit和Kulumsa站点的256、298、272和257 DOY。由ETCCDI开发的27个核心极端气候指数集已针对基线期和未来期进行了分析,本工作将详细讨论其中18个的结果。最低最低温度(TNn)的增加大于最高最高温度(TXx)的增加,最高最高温度(TXx)分别代表一年,季节或一个月中最冷或最热的日子。在两个RCP下,所有研究地点的日温度高于25ºC(称为夏季(SU25))的年度天数将大大增加,而最低温度低于0ºC的霜冻天数将减少。总体而言,极端温度指数表明,在本世纪中叶,所有研究地点的极端温度均在增加,而极端温度则在下降,这一序列清楚地表明了明显的变暖。从极端降水量来看,在Asasa的RCP4.5下,连续干旱天数(CDD)呈下降趋势,而在RCP8.5下,连续干旱日数呈上升趋势,而在Kulumsa地区则观察到该指数的反向趋势。

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