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首页> 外文期刊>Theoretical and applied climatology >Flood/drought event identification using an effective indicator based on the correlations between multiple time scales of the Standardized Precipitation Index and river discharge
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Flood/drought event identification using an effective indicator based on the correlations between multiple time scales of the Standardized Precipitation Index and river discharge

机译:基于标准化降水指数多个时标与河流流量之间的相关性,使用有效指标识别洪水/干旱事件

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摘要

In order to further investigate the capability of the Standardized Precipitation Index (SPI) to identify flood/drought events, monthly precipitation data from 26 precipitation stations and monthly discharge data from four hydrological stations from 1960 to 2006 in the Minjiang River basin were used to analyze the correlations between multiple time scales of the SPI and river discharge. The SPI series that had a maximum correlation with discharge was chosen to detect flood/drought events in the basin, and the results were compared to historical flood/drought events. The results indicated the following. (1) High Pearson correlations between the SPI and discharge were identified at shorter time scales (1 to 3 months), and the maximum correlation was found on the time scale of 2 months. (2) Five floods among the six largest historical flood events in the Minjiang River basin were identified with the 2-month SPI, but the SPI does have shortcomings in identifying more general floods. The SPI also identified major drought events that were consistent with historical data. This demonstrates that the 2-month SPI is an effective indicator for the identification of major flood/drought events in the Minjiang River basin.
机译:为了进一步研究标准降水指数(SPI)识别洪水/干旱事件的能力,利用the江流域1960年至2006年的26个降水站的月降水数据和4个水文站的月流量数据进行了分析。 SPI的多个时间尺度与河流流量之间的相关性。选择与流量最大相关的SPI系列来检测流域的洪水/干旱事件,并将结果与​​历史洪水/干旱事件进行比较。结果表明如下。 (1)在较短的时间范围内(1-3个月),可以确定SPI与放电之间的高Pearson相关性,而在2个月的时间范围内发现最大的Pearson相关性。 (2)month江流域的6个最大历史洪水事件中有5个洪水是通过2个月的SPI确定的,但是SPI在识别更多普通洪水方面确实存在不足。 SPI还确定了与历史数据一致的重大干旱事件。这表明,为期2个月的SPI是识别Min江流域重大洪水/干旱事件的有效指标。

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  • 来源
    《Theoretical and applied climatology》 |2017年第2期|159-168|共10页
  • 作者单位

    Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China|State Key Lab Humid Subtrop Mt Ecol, Cultivat Base, Fuzhou 350007, Peoples R China|Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou 350007, Peoples R China;

    Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China|State Key Lab Humid Subtrop Mt Ecol, Cultivat Base, Fuzhou 350007, Peoples R China|Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou 350007, Peoples R China;

    Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China|State Key Lab Humid Subtrop Mt Ecol, Cultivat Base, Fuzhou 350007, Peoples R China|Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou 350007, Peoples R China;

    Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China|State Key Lab Humid Subtrop Mt Ecol, Cultivat Base, Fuzhou 350007, Peoples R China|Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou 350007, Peoples R China;

    Fujian Normal Univ, Coll Geog Sci, Fuzhou 350007, Peoples R China|State Key Lab Humid Subtrop Mt Ecol, Cultivat Base, Fuzhou 350007, Peoples R China|Fujian Prov Engn Res Ctr Monitoring & Assessing T, Fuzhou 350007, Peoples R China;

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