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首页> 外文期刊>World Journal of Environmental Engineering >Spatio-temporal Drought Characterization for the Upper Tana River Basin, Kenya Using Standardized Precipitation Index (SPI)
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Spatio-temporal Drought Characterization for the Upper Tana River Basin, Kenya Using Standardized Precipitation Index (SPI)

机译:肯尼亚塔纳河流域上游时空干旱特征的标准化降水指数(SPI)

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Drought occurrence in the upper Tana River basin in Kenya has impacted negatively on water resources, hydro-power generation and agricultural production within the basin. Although this is an important river basin in Kenya, there is limited research work that has been done to assess and characterize drought to provide feasible mitigation measures and /or coping mechanics for water resources management. The Standardized Precipitation Index (SPI) was used to assess the spatio-temporal drought characteristics within the upper Tana River basin based on precipitation data for 41 years for eight gauging stations within the basin. The Kriging interpolation technique was applied to estimate spatially drought occurrence within the basin while the non-parametric Mann-Kendall (MK) trend test was used for trend detection. Results show that the south-eastern parts of the basin exhibit the highest drought severities while the north-western parts have the lowest drought values with averages of 2.140 and 4.065, and 2.542 and 4.812 in 1970 and 2010 respectively. The areal-extend of drought severities in both the south-eastern and north-western areas increased from 4868.7 km2 to 6880 km2, and 6163.9 km2 to 6985.5 km2 from 1970 to 2010 respectively. The drought trend increased in the south-eastern parts of the basin at 90% and 95% significant levels while no significant trend was detected in the north-western areas. The results presented in this paper are useful in formulating a drought early warning system that can be used to assist water resources managers in developing timely mitigation measures in planning and managing water resources within the basin.
机译:肯尼亚塔纳河上游流域发生的干旱对流域内的水资源,水力发电和农业生产产生了负面影响。尽管这是肯尼亚重要的流域,但为评估干旱和干旱特征而进行的研究工作有限,无法为水资源管理提供可行的缓解措施和/或应对机制。根据塔那河流域内八个测量站41年的降水数据,使用标准降水指数(SPI)评估塔纳河上游流域的时空干旱特征。应用Kriging插值技术估算流域内的空间干旱发生率,同时使用非参数Mann-Kendall(MK)趋势检验进行趋势检测。结果表明,该盆地东南部的干旱严重程度最高,而西北部的干旱值最低,1970年和2010年的平均干旱水平分别为2.140和4.065、2.542和4.812。 1970年至2010年,东南部和西北部干旱严重程度的面积范围分别从4868.7 km2增加到6880 km2,从6163.9 km2增加到6985.5 km2。流域东南部的干旱趋势以90%和95%的显着水平增加,而西北地区未发现显着趋势。本文提出的结果可用于制定干旱预警系统,该系统可用于协助水资源管理人员制定及时的缓解措施,以规划和管理流域内的水资源。

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