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Using a hydrological model to determine the cause of the water supply crisis for the town of Pernik in Bulgaria

机译:利用水文模型确定保加利亚佩尔尼克镇供水危机的原因

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In 2019 the Studena reservoir, the only water supply source for the town of Pernik in Bulgaria, accumulated less than half of its normal annual inflow. This factor, together with an inadequate and delayed response by the water resource managers caused a severe water supply crisis in the fall and winter of that year. As this situation was unprecedented, investigations were undertaken to determine the cause of the low inflow to the reservoir using the model CLM3 and available climatic and spatial data, and data that were collected in the watershed for the reservoir. The study was conducted by simulating the hydrological processes that take place in the watershed, and the monthly inflows to the reservoir for the period 2017-2019. It was found that hydrological parameters produced in the calibrated model were similar to those measured in the field and by another model. The achieved agreement was considered to be satisfactory given the complexity of their nature and assessment methods. The result of the study convincingly confirmed that the main reason for the poor inflow to the reservoir in 2019 was the low precipitation in this year and, above all, the scarce snowfall in the winter months. Although the total annual precipitation falling in the region during the period 2017-2019 has not changed significantly, but the seasonal distribution of precipitation has changed. In particular, the amount of precipitation that falls in snowfalls has declined and reached a minimum in 2019. These decreases are due to the increase in the average air temperature of 1 degrees C which causes the observed decreases in the runoff.
机译:2019年,Sechena水库,保加利亚普林尼克镇的唯一供水来源,累计不到其正常年度流入的一半。该因素与水资源经理的不充分和延迟的响应,在那年秋季和冬季导致了严重的供水危机。由于这种情况前所未有,因此进行了调查,以利用模型CLM3和可用气候和空间数据,以及在水库的流域收集的数据来确定低流入的原因。该研究是通过模拟流域发生的水文过程进行的,并为2017 - 2019年期间的水库流入。结果发现,校准模型中产生的水文参数与现场测量的水学参数和另一个模型类似。考虑到其性质和评估方法的复杂性,所取得的协议被认为是令人满意的。研究结果令人信服地证实,2019年对水库流入的主要原因是今年的降水量低,最重要的是,冬季的稀缺降雪。虽然2017 - 2019年期间在该地区的年度降水量落在该地区,但降水量的季节性分布已经发生变化。特别是,降雪量的降水量下降并在2019年达到了最低限度。这些降低是由于1摄氏度的平均气温的增加,导致径流中观察到的降低。

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