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Climate Change in Afghanistan Deduced from Reanalysis and Coordinated Regional Climate Downscaling Experiment (CORDEX)—South Asia Simulations

机译:通过重新分析和协调的区域气候缩减实验(CORDEX)推断的阿富汗气候变化—南亚模拟

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Past and the projected future climate change in Afghanistan has been analyzed systematically and differentiated with respect to its different climate regions to gain some first quantitative insights into Afghanistan’s vulnerability to ongoing and future climate changes. For this purpose, temperature, precipitation and five additional climate indices for extremes and agriculture assessments (heavy precipitation; spring precipitation; growing season length (GSL), the Heat Wave Magnitude Index (HWMI); and the Standardized Precipitation Evapotranspiration Index (SPEI)) from the reanalysis data were examined for their consistency to identify changes in the past (data since 1950). For future changes (up to the year 2100), the same parameters were extracted from an ensemble of 12 downscaled regional climate models (RCM) of the Coordinated Regional Climate Downscaling Experiment (CORDEX)-South Asia simulations for low and high emission scenarios (Representative Concentration Pathways 4.5 and 8.5). In the past, the climatic changes were mainly characterized by a mean temperature increase above global level of 1.8 °C from 1950 to 2010; uncertainty with regard to reanalyzed rainfall data limited a thorough analysis of past changes. Climate models projected the temperature trend to accelerate in the future, depending strongly on the global carbon emissions (2006–2050 Representative Concentration Pathways 4.5/8.5: 1.7/2.3 °C; 2006–2099: 2.7/6.4 °C, respectively). Despite the high uncertainty with regard to precipitation projections, it became apparent that the increasing evapotranspiration is likely to exacerbate Afghanistan’s already existing water stress, including a very strong increase of frequency and magnitude of heat waves. Overall, the results show that in addition to the already extensive deficiency in adaptation to current climate conditions, the situation will be aggravated in the future, particularly in regard to water management and agriculture. Thus, the results of this study underline the importance of adequate adaptation to climate change in Afghanistan. This is even truer taking into account that GSL is projected to increase substantially by around 20 days on average until 2050, which might open the opportunity for extended agricultural husbandry or even additional harvests when water resources are properly managed.
机译:对阿富汗过去和未来的气候变化进行了系统的分析,并针对其不同的气候区域进行了区分,以初步了解阿富汗对当前和未来气候变化的脆弱性。为此,需要温度,降水和另外五个用于极端和农业评估的气候指数(强降水,春季降水,生长期长度(GSL),热浪幅值指数(HWMI)和标准降水蒸散指数(SPEI))从重新分析中获得的数据进行了一致性检查,以确定过去的变化(自1950年以来的数据)。对于未来的变化(到2100年),从低和高排放情景的协调区域气候缩减实验(CORDEX)-南亚模拟的12个缩减区域气候模型(RCM)集合中提取了相同的参数(代表浓度途径4.5和8.5)。过去,气候变化的主要特征是从1950年到2010年,平均温度升高超过全球平均水平1.8°C。重新分析的降雨数据的不确定性限制了对过去变化的透彻分析。气候模型预测,未来温度趋势将加速增长,这在很大程度上取决于全球碳排放量(2006–2050年代表性浓度途径4.5 / 8.5:1.7 / 2.3°C; 2006–2099:2.7 / 6.4°C)。尽管降水预测存在高度不确定性,但显而易见的是,蒸散量的增加很可能加剧阿富汗已经存在的水资源压力,包括热浪频率和强度的大幅增加。总体而言,结果表明,除了对当前气候条件的适应已经很广泛的不足之外,将来,尤其是在水资源管理和农业方面,这种情况还会加剧。因此,这项研究的结果强调了充分适应阿富汗气候变化的重要性。考虑到GSL预计到2050年平均将平均增加20天左右,这更加正确,这可能会在适当管理水资源的情况下为扩大农业规模甚至增加收成提供机会。

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