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首页> 外文期刊>Hydrology and Earth System Sciences >Modelling the water budget and the riverflows of the Maritsa basin in Bulgaria
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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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A soil-vegetation-atmosphere transfer model coupled with a macroscaledistributed hydrological model was used to simulate the water cyclefor a large region in Bulgaria. To do so, an atmospheric forcing was builtfor two hydrological years (1 October 1995 to 30 September 1997), at an eight kmresolution. The impact of the human activitieson the rivers (especially hydropower or irrigation) was taken into account.An improvement of the hydrometeorological model was made: for better simulation of summerriverflow, two additional reservoirs were added to simulate the slowcomponent of the runoff. Those reservoirs were calibrated using the observeddata of the 1st year, while the 2nd year was used for validation.56 hydrologic stations and 12 dams were used for the model calibration while41 river gauges were used for the validation of the model. The results comparewell with the daily-observed discharges, with good results obtained overmore than 25% of the river gauges. The simulated snow depth was compared todaily measurements at 174 stations and the evolution of the snow waterequivalent was validated at 5 sites. The process of melting and refreezingof snow was found to be important in this region. The comparison of thenormalized values of simulated versus measured soil moisture showed goodcorrelation. The surface water budget shows large spatial variations due tothe elevation influence on the precipitation, soil properties andvegetation variability. An inter-annual difference was observed in the watercycle as the first year was more influenced by Mediterranean climate, whilethe second year was characterised by continental influence. The energy budgetshows a dominating sensible heat component in summer, due to the fact thatthe water stress limits the evaporation. This study is a first step for theimplementation of an operational hydrometeorological model that could beused for real time monitoring and forecasting of water budget components andriver flow in Bulgaria.
机译:保加利亚-大区域的土壤-植被-大气迁移模型与宏观分布式水文模型相结合,用于模拟水循环。为此,在两个水文年(1995年10月1日至1997年9月30日)建立了大气强迫,分辨率为8 km。考虑了人类活动对河流(特别是水力发电或灌溉)的影响。对水文气象模型进行了改进:为了更好地模拟夏季河水流,增加了两个额外的水库来模拟径流的慢分量。这些水库使用第一年的观测数据进行校准,而使用第二年进行验证。模型验证使用了56个水文站和12个大坝,模型验证使用了41个水位计。结果与每日观察到的流量相比较,在超过25%的河流水位上获得了良好的结果。将模拟的积雪深度与174个站点的每日测量值进行比较,并在5个站点上验证了雪水当量的演变。人们发现,该地区融雪和重新冻结的过程非常重要。模拟和实测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,土壤性质和植被变异性的影响,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,而第二年则受到大陆性影响,因此在水循环中观测到年际差异。由于水分胁迫限制了蒸发的事实,夏季能源预算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要素和驱动因素。

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