大多数湖泊模型及其与监测的联系

V. Vančura, L. Otte, L. Kruzikova, J. Gottfried, Z. Seliga
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摘要

原煤矿Ležáky-Most的区域,正在通过水力土地复垦过程变成Most湖,位于北波西米亚褐煤盆地的中部,Most镇以北,Unipetrol Orlen集团有限公司厂房以南。采石场的西南、南侧和东侧被捷克中央山脉(Hněvín, Špičák a Červený vrch)的剥蚀火山高地所包围。Ležáky-Most采石场占地1264公顷。其中,Most湖占地311.1公顷。水库蓄水量的稳定性主要取决于库区的气候特征,以及库区的天气条件。有必要更好地认识这些因素对命题模型的影响,并对其进行量化。我们的目的是建立一个能够预测湖泊水位变化的模型。本文总结了关于莫斯特湖的基本事实以及建立动态模型所必需的理论前提。正在定义模型,并收集量化模型变量所需的数据。项目团队的目标是创建一个全面的平衡模型来描述Most湖的水位行为。因此,监测系统的基本任务是在大多数湖泊模型中使用。本文将描述监视信息的可能性及其与模型的连接。
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Model of Most lake and its connection with monitoring
The area of the former coal mine Ležáky-Most, which is being turned into Lake Most by the process of hydric land reclamation, is located in the central part of the North-Bohemian brown coal basin, north of the town of Most, and south from the plant premises of Unipetrol Orlen Group, Ltd. From the southwest, south and east side the quarry is surrounded by denudated volcanic elevations of Czech Central Mountains - Hněvín, Špičák a Červený vrch. Ležáky-Most Quarry covers an area of 1264 hectares. Of this total, Lake Most will occupy 311.1 hectares. The stability of water capacity in reservoir Lake Most how about consequently altitude its surface is in his essence dependent on character of climate, plus as well on weather conditions in solving region. It is necessary better recognize these influence to proposition model as well as them quantify. Our intention is to create a model capable of predicting the lake water level behavior. This article summarizes the basic facts about Lake Most and theoretical prerequisites necessary for the creation of a dynamic model. The model is being defined and data necessary to quantify the model variables is being collected. The goal of the project team is to create a comprehensive balance model describing the water level behavior in Lake Most. That is why, the basic task of monitoring system is use in model of Most lake. This article will description possibilies monitoring informations and its connection to model.)
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