首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Hydrological simple water balance modeling for increasing geographically isolated doline wetland functions and its application to climate change
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Hydrological simple water balance modeling for increasing geographically isolated doline wetland functions and its application to climate change

机译:增加地理上孤立的Doline湿地功能的水文简单水平衡模型及其在气候变化中的应用

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In this study, we investigate the hydro-meteorological and hydro-geomorphological factors that influence the formation of wetlands in the doline. To this end, a set of ordinary differential equations are drawn to represent hydrological responses to hydro-meteorological forcings in wetland catchments and wetlands. The relative influence of hydro-meteorological forcings and hydro-geomorphological parameters on hydrological circulation in wetlands is explored through simple water balance models that reflect key hydrological processes in wetland catchments and wetlands. Among the hydro-geomorphological parameters of wetland catchments, the surface runoff coefficient have been found to play the most important role in determining inflow into wetlands. Among the hydro-geomorphological parameters of wetlands, we found that the relative size of the wetland area to the surrounding wetland catchment area and the exfiltration capacity at the wetland bottom have a significant effect on the formation and persistence of the doline wetland. These findings suggest that in-depth management of surface runoff in wetland catchments and the prevention of wetland bottom damage are critical for the conservation of doline wetlands. In addition, it is found that rainfall in doline wetlands in Korea has a much greater influence on wetland hydrological circulation than potential evapotranspiration. It is analyzed that the seasonality of rainfall has the greatest effect on wetland formation and persistence under general hydro-geomorphological conditions due to the nature of monsoon climate in Korea. Applying various future climate change scenario ensembles, it is projected that general doline wetlands will not be significantly affected by future climate change. However, it is revealed that doline wetlands, which are in a relatively good environment, are likely to be sensitive to future climatic conditions.
机译:在这项研究中,我们调查了影响丁醇中湿地形成的水力气象和水​​力正面因素。为此,绘制了一组普通微分方程,以代表湿地集水区和湿地的水力气象强制进行水文反应。通过简单的水平衡模型探讨了水力 - 气象强制对湿地水文循环的相对影响,反映了湿地集水区和湿地的关键水文过程。在湿地流域的水力 - 地貌参数中,已经发现表面径流系数在确定流入湿地方面发挥着最重要的作用。在湿地的水力 - 地貌参数中,我们发现湿地区域的相对大小与周围的湿地集水区和湿地底部的灭射能力对多丝湿地的形成和持续存在显着影响。这些研究结果表明,深入管理湿地集水区中的表面径流和防止湿地底部损坏对于养护湿地的保护至关重要。此外,还发现韩国多机湿地的降雨对湿地水文循环的影响大得多,而不是潜在的蒸发。分析,由于韩国季风气候的性质,降雨量的季节性对湿地形成和持久性的影响最大。应用各种未来的气候变化情景集合,预计将会受到未来气候变化的大大影响一般的多乐湿地。然而,据透露,在相对良好的环境中,Doline湿地可能对未来的气候条件敏感。

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