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Hydro-Meteorological Trends in the Upper Omo-Ghibe River Basin, Ethiopia

机译:埃塞俄比亚上部奥莫 - 甘地河流域的水力气象趋势

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This study aimed to assess trends of hydro-meteorological variables in the Upper Omo-Ghibe river basin, Ethiopia. Data records from eleven rainfall, eight air temperature, and five streamflow stations between 1981 to 2008 were investigated. The trends and change points were evaluated for different periods of time depending on data availability. Mann-Kendall and Pettit tests were used to identify trends and change points at a 5% significance level. The tests were applied to mean annual, monthly and seasonal time scales. Rainfall exhibited statistically decreasing trends at a mean annual time scale, while seasonal rainfall depicted heterogeneous results in both directions. For the majority of the stations, air temperature showed statistically significant increasing trends. The magnitude of change in temperature for mean annual, wet and dry season has increased about 0.48, 0.46, and 0.61 °C per decade for Jimma station. The Pettit test revealed that the late 1980s and 1990s were the change points. There is generally a decreasing trend in streamflow. The decline in annual rainfall and rise in temperature affected the streamflow negatively. Overall, the results indicate that trend sand change point times varied considerably across the stations and catchments. The identified significant trends can help to support planning decisions for water management.
机译:本研究旨在评估埃塞俄比亚上部Omo-Ghibe河流域水力气象变量的趋势。研究了1981年至2008年之间的十一降雨,八个空气温度和五个流出站的数据记录。根据数据可用性对不同的时间段进行评估趋势和变化点。 Mann-Kendall和Pettit测试用于识别5%的重要性水平的趋势和变化点。测试应用于平均年度,每月和季节性尺度。降雨表现出统计上的年度尺度统计上减少趋势,而季节性降雨已经描绘了两个方向的异质导致。对于大多数车站来说,空气温度显示出统计上显着的趋势。对于吉米站,平均年度,湿季节,湿季节,湿季节,湿季节的温度变化的大小增加了0.48,0.46和0.61°C。 Pettit测试显示,20世纪80年代后期和1990年代是变化点。流出的趋势通常在流出中。年降雨量下降,温度升高影响了流出的负面流。总的来说,结果表明,趋势沙变化点时代在站点和集水区内各种各样地变化。确定的重大趋势可以帮助支持水资管理的规划决策。

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