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气候变化对巴拉顿湖(匈牙利)径流和溶解性磷负荷的影响。

Impacts of the climate change on runoff and diffuse phosphorus load to Lake Balaton (Hungary).

作者信息

Kovács A, Clement A

机构信息

Department of Sanitary and Environmental Engineering, Budapest University of Technology and Economics, Budapest, Hungary.

出版信息

Water Sci Technol. 2009;59(3):417-23. doi: 10.2166/wst.2009.883.

Abstract

The paper outlines a multi-component assessment of the impacts of the climate change on runoff and total phosphorus loads to the large shallow Lake Balaton in Hungary. Present hydrological cycle of the lake catchment has been examined using the rainfall-runoff model WetSpa. Particular phosphorus concentration in runoff was estimated on the basis of the simulated streamflow using an empirical power equation. Dissolved phosphorus concentrations were determined as a function of landuse and soil type of the corresponding sub-catchment. The model was calibrated and validated against daily observations manually at monitoring sites of sixteen inflowing streams around the lake. Runoff stemming from shoreline urban developments was calculated by the urban runoff simulation model SWMM. Phosphorus concentrations in urban runoff were calculated by an empirical relationship derived from field measurements. The model was henceforward run for climate change scenario analysis. Present weather data were modified by the climate change scenarios imported from the results of the CLIME project. The results indicate that the impact of the climate change on runoff and phosphorus load appears in the change of the distribution within a time period rather than in the total volume. However, due to the high uncertainties in climate models, the presented calculations are possible assumptions rather than established statements.

摘要

该论文概述了对气候变化对匈牙利大浅湖巴拉顿湖径流和总磷负荷影响的多要素评估。利用降雨径流模型WetSpa研究了该湖集水区当前的水文循环。基于模拟的河川径流,使用经验幂方程估算径流中的特定磷浓度。溶解磷浓度根据相应子集水区的土地利用和土壤类型确定。该模型针对该湖周围16条流入溪流监测点的每日观测数据进行了人工校准和验证。通过城市径流模拟模型SWMM计算来自海岸线城市发展的径流。城市径流中的磷浓度通过现场测量得出的经验关系计算。此后该模型用于气候变化情景分析。当前天气数据根据从CLIME项目结果导入的气候变化情景进行了修改。结果表明,气候变化对径流和磷负荷的影响表现为一段时间内分布的变化,而非总量的变化。然而,由于气候模型存在高度不确定性,所呈现的计算结果只是可能的假设,而非既定结论。

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