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Sensitivity of the West African hydrological cycle in ORCHIDEE to infiltration processes

机译:西非水文循环在ORCHIDEE中对入渗过程的敏感性

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The aim of this article is to test the sensitivity of the West Africanhydrological cycle to infiltration processes and to riverreinfiltration pathways. This is done through sensitivity experimentsto both inputs and paramterization settings of the ORCHIDEELand-Surface Model. The parameterizations to take into account the effects of flat areas, pondsand floodplains on surface infiltration, and the effect of roots anddeep-soil compactness on infiltration are first described. The sensitivityanalysis to parameterization settings shows that the surface infiltration processes have a stronger impact in thesoudano-sahelian region and more generally in semi-arid African regions, whereas the rootzone and deep-soilinfiltration also play a role in the guinean and intermediate regions between arid and humid ones. In the equatorialand semi-humid regions, infiltration processes generally play a minor role. The infiltrationparameterizations may explain part of the difference between simulated and observed river discharge in semi-aridand intermediate basins. The sensitivity analysis to the Land-SurfaceModel inputs shows that different sources of uncertainty might also explain part of the error.Indeed, the precipitation forcing in the whole West African region, the long-term storage in thesoudano-sahelian region, the soil types in the guinean region andthe vegetation types in the equatorial region are significant sources oferrors. Therefore, observations and analyses of small scale infiltration processes aswell as continuous measurements of river discharges in West Africa areessential to ensure the reliability of futurecalibration for the infiltration parameterizations.
机译:本文的目的是测试西非水文循环对入渗过程和河流再入途径的敏感性。这是通过对ORCHIDEEL和曲面模型的输入和参数设置进行敏感性实验来完成的。首先描述了考虑平坦区域,池塘和洪泛区对表层入渗的影响以及根和深层土壤密实度对入渗的影响的参数化。对参数设置的敏感性分析表明,地表入渗过程在苏达诺-萨赫勒地区和更普遍的非洲半干旱地区具有更强的影响,而根区和深层土壤入渗在几内亚和几内亚之间的干旱和中间地区也起作用。潮湿的。在赤道半湿润地区,渗透过程通常起着较小的作用。入渗参数化可以解释半干旱和中游盆地模拟河流流量与观测河流流量之间的部分差异。对Land-SurfaceModel输入的敏感性分析表明,不确定性的不同来源也可能解释了部分误差。实际上,整个西非地区的降水强迫,soudano-sahelian地区的长期储藏,土壤类型几内亚地区和赤道地区的植被类型是重要的误差来源。因此,对小规模入渗过程的观察和分析以及对西非河流流量的连续测量对于确保未来渗透参数化校准的可靠性至关重要。

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