首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >Simulating water temperatures and stratification of a pre‐alpine lake with a hydrodynamic model: calibration and sensitivity analysis of climatic input parameters
【24h】

Simulating water temperatures and stratification of a pre‐alpine lake with a hydrodynamic model: calibration and sensitivity analysis of climatic input parameters

机译:用水动力模型模拟前高山湖泊的水温和分层:气候输入参数的校准和敏感性分析

获取原文
获取原文并翻译 | 示例
           

摘要

We report on the calibration of the one-dimensional hydrodynamic lake model Dynamic Reservoir Simulation Model to simulate the water temperature conditions of the pre-alpine Lake Ammersee (southeast Germany) that is a representative of deep and large lakes in this region. Special focus is given to the calibration in order to reproduce the correct thermal distribution and stratification including the time of onset and duration of summer stratification. To ensure the application of the model to investigate the impact of climate change on lakes, an analysis of the model sensitivity under stepwise modification of meteorological input parameters (air temperature, wind speed, precipitation, global radiation, cloud cover, vapour pressure and tributary water temperature) was conducted. The total mean error of the calibration results is −0.23 °C, the root mean square error amounts to 1.012 °C. All characteristics of the annual stratification cycle were reproduced accurately by the model. Additionally, the simulated deviations for all applied modifications of the input parameters for the sensitivity analysis can be differentiated in the high temporal resolution of monthly values for each specific depth. The smallest applied alteration to each modified input parameter caused a maximum deviation in the simulation results of at least 0.26 °C. The most sensitive reactions of the model can be observed through modifications of the input parameters air temperature and wind speed. Hence, the results show that further investigations at Lake Ammersee, such as coupling the hydrodynamic model with chemo-dynamic models to assess the impact of changing climate on biochemical conditions within lakes, can be carried out using Dynamic Reservoir Simulation Model. Copyright © 2012 John Wiley & Sons, Ltd.
机译:我们报告一维水力动力学湖泊模型的动态水库模拟模型的校准,以模拟前高山湖泊Ammersee(德国东南部)的水温条件,该湖是该地区深,大湖泊的代表。为了重现正确的热分布和分层,包括开始的时间和夏季分层的持续时间,要特别注意校准。为了确保该模型可用于调查气候变化对湖泊的影响,在逐步修改气象输入参数(气温,风速,降水,全球辐射,云量,蒸气压和支流水)下对模型敏感性进行分析温度)。校准结果的总平均误差为-0.23°C,均方根误差为1.012°C。该模型准确地再现了年度分层周期的所有特征。另外,对于灵敏度分析,输入参数的所有应用修改的模拟偏差可以通过每个特定深度的月度值的高时间分辨率来区分。对每个修改后的输入参数的最小应用更改导致仿真结果的最大偏差至少为0.26°C。可以通过修改输入参数空气温度和风速来观察模型中最敏感的反应。因此,结果表明,可以使用动态水库模拟模型对Ammersee湖进行进一步的研究,例如将水动力学模型与化学动力学模型耦合以评估气候变化对湖泊内生化条件的影响。版权所有©2012 John Wiley&Sons,Ltd.

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号