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Comparing results of a remote sensing driven interception-infiltration model for regional to global applications with ECMWF data

机译:与ECMWF数据的区域到全局应用的遥感驱动拦截渗透模型的结果

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We present results of a remote sensing based modelling approach to simulate the 1D water transport in the vadose zone of unsaturated soils on a daily basis, which can be used for regional to global applications. To calculate the hydraulic conductivity our model is driven by van Genuchten parameters, which we calculated for Bavaria (South-East-Germany), which we choose as area of investigation, using the ISRIC-WISE Harmonized Global Soil Profile Dataset Ver. 3.1 and the Rosetta programme. Soil depth and layering of up to six layers were defined independently for each soil. Interception by vegetation is also considered by using Leaf Area Index (LAI) time series from SPOT-VEGETATION. Precipitation is based on daily time series from the European Centre for Medium-Range Weather Forecasts (ECMWF). The model was applied to the Biosphere Energy Transfer Hydrology (BETHY/DLR) vegetation model, driven at the German Aerospace Center (DLR), to discuss the possibility of regionalization of a global model concept, regarding the soil water budged. Furthermore we compare our results with ECMWF data and discuss the results for the state of Bavaria. We found a good agreement for the general characteristics of our results with this dataset, especially for soils which are close to the standard characteristics of the ECMWF. Disagreements were found for shallow soils and soils under stagnant moisture, which are not considered in the ECMWF modelling scheme, but are distinguished in our approach.
机译:我们在每日基础上呈现遥感基于遥感的建模方法的结果,以模拟不饱和土的Vadosose区中的1D水输送,可用于区域到全球应用。为了计算液压导电性,我们的模型由Van Genuchten参数驱动,我们计算为巴伐利亚(东南 - 德国),我们选择作为调查领域,使用Isric-Wise谐波的全球土壤剖面数据集Ver。 3.1和Rosetta计划。为每种土壤独立定义土壤深度和多达六层的层。通过使用点植被的叶面积指数(LAI)时间序列,还考虑植被的拦截。降水基于欧洲中等地区天气预报中心(ECMWF)的日常时间序列。该模型应用于生物圈能量转移水文(贝特/ DLR)植被模型,在德国航天中心(DLR)驱动,讨论了全球模型概念的区域化的可能性,关于土壤水衰竭。此外,我们将我们的结果与ECMWF数据进行比较,并讨论巴伐利亚州的结果。我们发现我们对该数据集的结果一般特征的一致意见,特别是对于接近ECMWF标准特征的土壤。发现浅层土壤和土壤中的分歧,停滞水分下,这在ECMWF建模方案中不考虑,但在我们的方法中区分。

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