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Synthetic Impacts of Internal Climate Variability and Anthropogenic Change on Future Meteorological Droughts over China

机译:内部气候变化和人为变化对中国未来气象干旱的综合影响

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The climate change impacts on droughts have received widespread attention in many recent studies. However, previous studies mainly attribute the changes in future droughts to human-induced climate change, while the impacts of internal climate variability (ICV) have not been addressed adequately. In order to specifically consider the ICV in drought impacts, this study investigates the changes in meteorological drought conditions for two future periods (2021–2050 and 2071–2100) relative to a historical period (1971–2000) in China, using two multi-member ensembles (MMEs). These two MMEs include a 40-member ensemble of the Community Earth System Model version 1 (CESM1) and a 10-member ensemble of the Commonwealth Scientific and Industrial Research Organization Mark, version 3.6.0 (CSIRO-Mlk3.6.0). The use of MMEs significantly increases the sample size, which makes it possible to apply an empirical distribution to drought frequency analysis. The results show that in the near future period (2021–2050), the overall drought conditions represented by drought frequency of 30- and 50-year return periods of drought duration and drought severity in China will deteriorate. More frequent droughts will occur in western China and southwestern China with longer drought duration and higher drought severity. In the far future period (2071–2100), the nationwide drought conditions will be alleviated, but model uncertainty will also become significant. Deteriorating drought conditions will continue in southwestern China over this time period. Thus, future droughts in southwestern China should be given more attention and mitigation measures need to be carefully conceived in these regions. Overall, this study proposed a method of taking into account internal climate variability in drought assessment, which is of significant importance in climate change impact studies.
机译:在许多最新研究中,气候变化对干旱的影响已引起广泛关注。但是,先前的研究主要将未来干旱的变化归因于人为引起的气候变化,而内部气候变率(ICV)的影响尚未得到充分解决。为了具体考虑ICV在干旱中的影响,本研究调查了相对于中国历史时期(1971-2000年)的两个未来时期(2021-2050年和2071-2100年)的气象干旱状况的变化,使用了两个成员乐团(MME)。这两个MME包括40个成员的社区地球系统模型版本1(CESM1)和10个成员的联邦科学与工业研究组织Mark版本3.6.0(CSIRO-Mlk3.6.0)。 MME的使用显着增加了样本量,这使得将经验分布应用于干旱频率分析成为可能。结果表明,在不久的将来(2021年至2050年),以30年和50年回归期的干旱频率和干旱严重程度为代表的中国整体干旱状况将恶化。中国西部和西南地区将发生更频繁的干旱,干旱持续时间更长,干旱严重程度更高。在不久的将来(2071-2100年),全国范围内的干旱条件将得到缓解,但是模型不确定性也将变得非常重要。在此期间,中国西南地区的干旱状况将继续恶化。因此,应该更多地关注中国西南地区未来的干旱,并在这些地区仔细考虑缓解措施。总体而言,这项研究提出了一种在干旱评估中考虑内部气候变异性的方法,这在气候变化影响研究中具有重要意义。

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