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BibEntryCargo > Volume: 19 & Note : Auto downloaded ref at: 2020-06-25 or Auto downloaded ref at: 2020-06-26

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A 2-D process-based model for suspended sediment dynamics: a first step towards ecological modeling (1) · A measure to cope with DEM scale dependence of topographic index within TOPMODEL (1) · A simulation and prediction of agricultural irrigation on groundwater in well irrigation area of the piedmont of Mt. Taihang, North China (1) · Avaliação do TOPMODEL na estimativa do escoamento superficial em microbacia hidrográfica em diferentes usos (1) · Conditioning model output statistics of regional climate model precipitation on circulation patterns (1) · Distribution of soil carbon stocks in Canada's forests and wetlands simulated based on drainage class, topography and remotely sensed vegetation parameters (1) · From runoff to rainfall: inverse rainfall–runoff modelling in a high temporal resolution (1) · How to model shallow water-table depth variations: the case of the Kervidy-Naizin catchment, France: MODELLING WATER TABLE DEPTH (1) · Hydrologic Impacts of Ensemble-RCM-Projected Climate Changes in the Athabasca River Basin, Canada (1) · Including the dynamic relationship between climatic variables and leaf area index in a hydrological model to improve streamflow prediction under a changing climate (1) · Model determination of non-point source phosphorus transport pathways in a fertilized grassland catchment (1) · Modeling suspended sediment sources and transport in the Ishikari River basin, Japan, using SPARROW (1) · Modeling the primary and secondary productions of the southern Benguela upwelling system: A comparative study through two biogeochemical models: SOUTHERN BENGUELA ECOSYSTEM MODELING (1) · Modelling nitrogen removal in potential wetlands at the catchment scale (1) · Origin of shallow groundwater of Csepel Island (south of Budapest, Hungary, River Danube): isotopic and chemical approach (1) · Parallel Computation of the Regional Ocean Modeling System (1) · Simulation of a groundwater fall caused by geological discontinuities (1) · The Temporal Variability of Soil Moisture and Surface Hydrological Quantities in a Climate Model (1)
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