基于标准化降水指数(SPI)和有效干旱指数(EDI)的肯尼亚上塔纳河流域气象干旱时空及趋势探测

R. Wambua, B. Mutua, J. Raude
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引用次数: 22

摘要

由于干旱对水资源的负面影响,世界各地的干旱事件正日益成为一个关键问题。为了规划缓解措施,需要了解现场干旱特征。本文利用标准化降水指数(SPI)和有效干旱指数(EDI)对塔纳河上游流域的气象干旱事件进行了空间、时间和趋势分析。本研究使用了8个气象站41年(1980-2016)的月降水量数据。SPI和EDI用于重建干旱事件,并用于表征干旱发生的空间、时间和趋势分布。干旱频率估计为确定的严重程度与其事件总数的比率。干旱事件的变化是使用非参数man-Kendall趋势检验来检测的。SPI和EDI检测到的主要干旱条件是严重干旱、中度干旱、接近正常、中度潮湿、非常潮湿和极度潮湿。从结果来看,1970年至2010年间,东南部和西北部地区的平均干旱频率分别为12.16%至14.93%和3.82%至6.63%。Mann-Kendall趋势测试表明,该盆地东南部的干旱趋势分别增加了90%和95%。然而,在西北地区没有发现明显的趋势。这表明,与塔纳河上游流域的西北地区相比,东南部地区更容易发生干旱。SPI和EDI在检测干旱现场、描述整个流域的时间变异性、严重程度和空间范围方面都是有效的。建议将研究结果用于流域干旱预警系统的决策。
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Detection of Spatial, Temporal and Trend of Meteorological Drought Using Standardized Precipitation Index (SPI) and Effective Drought Index (EDI) in the Upper Tana River Basin, Kenya
Drought events across the world are increasingly becoming a critical problem owing to its negative effects on water resources. There is need to understand on-site drought characteristics for the purpose of planning mitigation measures. In this paper, meteorological drought episodes on spatial, temporal and trend domains were detected using Standardized Precipitation Index (SPI) and Effective Drought Index (EDI) in the upper Tana River basin. 41 years (1980-2016) monthly precipitation data from eight meteorological stations were used in the study. The SPI and EDI were used for reconstruction of the drought events and used to characterize the spatial, temporal and trend distribution of drought occurrence. Drought frequency was estimated as the ratio of a defined severity to its total number of events. The change in drought events was detected using a non-parametric man-Kendall trend test. The main drought conditions detected by SPI and EDI are severe drought, moderate drought, near normal, moderate wet, very wet and extremely wet conditions. From the results the average drought frequency between 1970 and 2010 for the south-eastern and north-western areas ranged from 12.16 to 14.93 and 3.82 to 6.63 percent respectively. The Mann-Kendall trend test show that drought trend increased in the south-eastern parts of the basin at 90% and 95% significant levels. However, there was no significant trend that was detected in the North-western areas. This is an indication that the south-eastern parts are more drought-prone areas compared to the North-western areas of the upper Tana River basin. Both the SPI and the EDI were effective in detecting the on-set of drought, description of the temporal variability, severity and spatial extent across the basin. It is recommended that the findings be adopted for decision making for drought-early warning systems in the river basin.
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