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A multimodel assessment of drought characteristics and risks over the Huang-Huai-Hai River basin, China, under climate change

机译:在气候变化下,中国黄淮海河流域干旱特征和风险的多模型评估

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Drought has become one of the most serious meteorological disasters for agricultural production in many areas around the world, and the situation could be worse under the impact of climate change. To facilitate better adaptation planning, this study proposed a drought assessment framework integrating downscaling method, drought index, copula technique, and bivariate frequency analysis, and applied it to investigate the change of the drought characteristics and drought risks from the past to the future in Huang-Huai-Hai River basin (HRB), North China. Drought was firstly defined by standardized precipitation evapotranspiration index (SPEI) based on 1497 observed grid data from 1979 to 2004. Then, we constructed the joint distribution of drought duration and severity based on copulas to detect and quantify the drought risks. To address the effect of climate change, similar calculation process was applied to the future climate data, which was downscaled using delta change method from representative concentration pathway (RCP 8.5) of 12 general circulation models (GCMs). The study results suggested that, under climate change condition, most irrigation districts over HRB would generally experience lower frequency of drought events but with extended duration; some districts would have more serious drought, but majority would experience similar or even lower level of severity. In light of the mean joint occurrence probability, the irrigation district at the south part of Huai River basin would likely experience the highest increase of drought risks in near future (by 0.86%) and distant future (by 0.76%), while most of other districts over HRB would face low risk of serious drought risks. The obtained results offer useful information to agricultural managers or water resources authorities who are interested in the development of effective long-term adaptation strategies for drought management.
机译:干旱已成为全球许多地区农业生产最严重的气象灾害之一,在气候变化的影响下,情况可能会更糟。为了促进更好的适应计划,本研究提出了一项干旱评估框架,整合了缩小机制方法,干旱指数,Copula技术和双变频分析,并应用了探讨了从过去到未来的干旱特征和干旱风险的变化 - 华海河流域(HRB),华北地区。首先由1979年至2004年的1497年观察到的网格数据的标准化降水蒸发指数(SPEI)首先定义了干旱。然后,我们根据Copulas构建了干旱持续时间和严重程度的联合分布,以检测和量化干旱风险。为了解决气候变化的影响,将类似的计算过程应用于未来的气候数据,这是使用来自12个普通循环模型(GCMS)的代表性浓度途径(RCP 8.5)的Delta改变方法缩小。研究结果表明,在气候变化条件下,大多数灌区,超过HRB的灌溉区通常会经历较低的干旱事件的频率,但持续时间延长;一些地区会有更严重的干旱,但大多数人将经历类似甚至更低的严重程度。鉴于平均联合发生概率,淮河盆地南部的灌溉区可能会在不久的将来(0.86%)和遥远的未来(0.76%)的最高增长的干旱风险增加,而大多数其他人HRB的地区将面临严重干旱风险的低风险。获得的结果为有兴趣开发干旱管理有效长期适应策略的农业经理或水资源机构提供有用信息。

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