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首页> 外文期刊>Journal of Hydrology >Critical drought severity/intensity-duration-frequency curves based on precipitation deficit
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Critical drought severity/intensity-duration-frequency curves based on precipitation deficit

机译:基于降水缺陷的临界干旱严重程度/强度持续时间曲线

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Drought is one of the most disastrous natural phenomena that causes scarcity and lack of water in hydrological basins and affects seriously the majority of the population in many ways such as economical, social and environmental. Therefore, drought plays a significant role in the risk management of water resources systems. The purpose of this study is to develop the severity/intensity-duration-frequency curves based on precipitation deficit and provide a comprehensive characterization of droughts by using Standardized Precipitation Index (SPI) which considers precipitation data only. Instead of using SPI directly, the severity and intensity were calculated in the duration-frequency curves. On the other hand, SPI is a technical tool and thus difficult to understand at first glance by end-users and decision-makers. Precipitation deficit is therefore more useful and physically meaningful to the users. In this study, drought with the largest severity in each year is defined as the critical drought of the year. Frequency analysis is applied on the critical drought severity to determine the bestfit probability distribution function by using the total probability theorem. Results show that the 2 year-return period drought severity/intensity-duration-frequency curve is well lower than and separated clearly from the curves at higher return periods of 5-100 years although it has the same tendency with the longer return period curves, and also that almost no difference is observed between the precipitation deficit of the droughts of 25 years or longer return periods. With the precipitation deficit and such newly introduced concepts as critical drought severity, singular drought and within-period drought, the proposed methodology gains a novelty. It is expected that the destructive and irreversible effects of meteorological, agricultural and hydrological droughts can be realized in a more physical sense with the use of precipitation deficit.
机译:干旱是最灾难性的自然现象之一,导致水文盆地中的稀缺和缺乏水,并以经济,社会和环境的多种方式严重影响大多数人口。因此,干旱在水资源系统的风险管理中起着重要作用。本研究的目的是通过使用标准化降水指数(SPI)来发展基于降水缺陷的严重程度/强度持续时间曲线,并通过使用标准化降水指数(SPI)来提供干旱的综合表征,该标准化降水指数仅考虑降水数据。在持续时间曲线中计算严重性和强度而不是直接使用SPI。另一方面,SPI是一种技术工具,因此难以通过最终用户和决策者迈出难以理解。因此,降水赤字对用户更有用和物理上有意义。在这项研究中,每年具有最大严重程度的干旱被定义为今年的危急干旱。频率分析应用于临界干旱严重程度,通过使用总概率定理来确定最佳概率分布功能。结果表明,2年返回期干旱严重程度/强度持续时间频率曲线远低于且清晰地分开,避免在5-100岁的曲线上,尽管它具有相同的返回期曲线趋势,并且,在返回时间为25岁或更长时间的干旱降水缺损之间几乎没有差异。随着降水赤字和这种新引进的概念作为临时干旱严重程度,奇异的干旱和期间的干旱,所提出的方法获得了一种新颖性。预计通过使用降水缺陷,可以在更有物理意义上实现气象,农业和水文干旱的破坏性和不可逆转的影响。

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