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Modelling the water budget and the riverflows of the Maritsa basin in Bulgaria

机译:对保加利亚Maritsa盆地的水预算和河流流量进行建模

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摘要

A soil-vegetation-atmosphere transfer model coupled with a macroscale distributed hydrological model was used to simulate the water cycle for a large region in Bulgaria. To do so, an atmospheric forcing was built for two hydrological years (1 October 1995 to 30 September 1997), at an eight km resolution. The impact of the human activities on the rivers (especially hydropower or irrigation) was taken into account. An improvement of the hydrometeorological model was made: for better simulation of summer riverflow, two additional reservoirs were added to simulate the slow component of the runoff. Those reservoirs were calibrated using the observed data of the 1st year, while the 2nd year was used for validation. 56 hydrologic stations and 12 dams were used for the model calibration while 41 river gauges were used for the validation of the model. The results compare well with the daily-observed discharges, with good results obtained over more than 25% of the river gauges. The simulated snow depth was compared to daily measurements at 174 stations and the evolution of the snow water equivalent was validated at 5 sites. The process of melting and refreezing of snow was found to be important in this region. The comparison of the normalized values of simulated versus measured soil moisture showed good correlation. The surface water budget shows large spatial variations due to the elevation influence on the precipitation, soil properties and vegetation variability. An inter-annual difference was observed in the water cycle as the first year was more influenced by Mediterranean climate, while the second year was characterised by continental influence. The energy budget shows a dominating sensible heat component in summer, due to the fact that the water stress limits the evaporation. This study is a first step for the implementation of an operational hydrometeorological model that could be used for real time monitoring and forecasting of water budget components and river flow in Bulgaria.
机译:保加利亚-大区域的土壤-植被-大气转移模型与宏观分布式水文模型被用来模拟水循环。为此,在两个水文年(1995年10月1日至1997年9月30日)以8公里的分辨率建立了大气强迫。考虑了人类活动对河流(尤其是水力发电或灌溉)的影响。改进了水文气象模型:为了更好地模拟夏季河水,增加了两个额外的水库来模拟径流的缓慢分量。这些储层使用第一年的观测数据进行了校准,而第二年用于验证。 56个水文站和12个大坝用于模型校准,而41个水位计用于模型验证。结果与每日观察到的排放量比较好,在超过25%的河流水位上都获得了良好的结果。将模拟的积雪深度与174个站点的每日测量值进行了比较,并在5个站点验证了雪水当量的演变。人们发现,雪的融化和重新冻结过程在该地区很重要。模拟土壤水分与测量土壤水分的标准化值的比较显示出良好的相关性。由于海拔高度对降水,土壤特性和植被变化的影响,地表水收支表现出较大的空间变化。由于第一年受地中海气候的影响较大,而第二年受大陆影响,因此水循环中存在年际差异。由于水分胁迫限制了蒸发,因此能源预算在夏季显示出显着的显热成分。这项研究是实施可操作的水文气象模型的第一步,该模型可用于实时监测和预测保加利亚的水预算组成部分和河流流量。

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