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Impact of Climate Change on Precipitation in Zambeze River Basin in Southern Africa

机译:非洲南部赞比西河流域气候变化对降水的影响

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The Intergovernmental Panel on Climate Change (IPCC) concluded that there is a consensus that the increase in atmospheric greenhouse gases will result in climate change, which will cause the sea level to rise, increase frequency of extreme climatic events such as intense storms, heavy rainfall events and droughts. This will increase the frequency of climate-related hazards, causing loss of life, social disruption and economic hardships. There is less consensus on the magnitude of change of climatic variables, nonetheless several studies have shown that climate change will have an impact on the availability and demand for water resources. Southern Africa lies in one of the regions of the world that is most susceptible to climate variability and change. In southern Africa, climate change is likely to affect nearly every aspect of human well-being, from agricultural productivity and energy use to flood control, municipal and industrial water supply as well as wildlife management, since the region is characterized by highly spatial and temporally variable rainfall, and in some cases, scarce water resources. This study presents the future change projection in precipitation under RCP2.6, RCP4.5 and RCP8.5 scenarios of the CanESM2 outputs using the Statistical Downscaling Model (SDSM) for 50 stations in Zambeze River basin during the two future periods: near future (2031-2060) and far future (2071-2100). For assessment of climate change, the baseline period (1979-2013) was partitioned into two periods for SDSM calibration (1979-1996) and validation (1997-2013). The results show that SDSM was not a very robust method for the simulation of precipitation for this study area, the model could not replicate observed precipitation very well. This is due to its conditional nature and high variability in space. The results also showed that there is a decrease in monthly precipitation during wet period (October-March) and an increase during the dry period (April-September). The upward monthly increase in projected precipitation expected is in August (300%, 325%) with RCP4.5 and maximum decrease in March (38%) with RCP4.5 for all scenarios for NF and FF respectively, and the projected annual precipitation is expected to decrease with time for all scenarios. It was observed that the maximum decrease will range from 7-21.8% for near future (NF) and 2-21% for far future (FF).
机译:政府间气候变化专门委员会(IPCC)得出结论认为,大气温室气体的增加将导致气候变化,这将导致海平面上升,极端气候事件(如强风暴,暴雨)的发生频率增加,这是共识事件和干旱。这将增加与气候有关的危害的发生频率,造成生命损失,社会破坏和经济困难。关于气候变量变化幅度的共识尚少,尽管有几项研究表明,气候变化将对水资源的供应和需求产生影响。南部非洲位于世界上最容易受到气候变化和变化影响的地区之一。在南部非洲,气候变化可能会影响人类福祉的几乎所有方面,从农业生产力和能源使用到防洪,市政和工业用水以及野生动植物管理,因为该地区的特点是时空高度降雨不定,在某些情况下水资源稀缺。本研究使用统计降尺度模型(SDSM)针对两个未来时期的赞比西河流域的50个台站提供了CanESM2输出的RCP2.6,RCP4.5和RCP8.5情景下降水的未来变化预测: 2031-2060)和遥远的未来(2071-2100)。为了评估气候变化,将基线期(1979-2013年)分为两个时期,分别用于SDSM校准(1979-1996年)和验证(1997-2013年)。结果表明,SDSM不是该研究区域降水模拟的非常可靠的方法,该模型不能很好地复制观测到的降水。这是由于其条件性质和空间的高度可变性。结果还表明,湿润时期(10月至3月)的月降水量减少,而干燥时期(4月至9月)的月降水量增加。对于NF和FF的所有情景,预期降水量在8月份分别为8月(300%,325%)和3月最大降幅(38%)(RCP4.5)。在所有情况下,预计都会随着时间而减少。据观察,最大的下降幅度在近期(NF)范围内为7-21.8%,对于远期(FF)范围为2-21%。

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