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chapter describes the hydrologic processes that affect the generation of streamflow in British Columbia's watersheds. These processes include precipitation, interception, evaporation, infiltration, soil mois- ture storage and hillslope flow, overland flow, and groundwater. The processes and their spatial and temporal variability
Hydrologic Components: Rainfall or Snow. Interception. Depression storage. Evapotranspiration. Infiltration. Surface storage. Runoff. Interflow. Groundwater flow adapted from EPA BASINS workshop. Evapotranspiration. Interception. Depression storage. Ground surface. Capillary rise. Precipitation. Infiltration. Soil moisture.
Hydrologic Processes. ? Hydrologic information – for planning and management of watersheds. ? Hydrologically watershed conceptualized – Precipitation ->. Runoff: Evaporation Transpiration. Runoff: Evaporation, Transpiration,. Interception, Infiltration etc. ? Watershed: Overland flow, Channel flow & subsurface flow
Hydrologic Processes. NORMAN E. PETERS. 9.1 INTRODUCTION. A catchment is a basic unit of landscape particularly for investigations of hydro- logic processes. Typically,the topographic boundary of a catchment coincides with the hydrologic boundary causing any precipitation falling on to the catchment to be routed to
atmosphere, oceans, lakes, rivers, soils, glaciers, snowfields, and groundwater. Water moves from one reservoir to another by way of processes like evaporation, condensation, precipitation, deposition, runoff, infiltration, sublimation, transpira- tion, melting, and groundwater flow. The oceans supply most of the evaporated
Introduction to Hydrology. 1) Definition and scope of Hydrology. 2) Examples of water resources and engineering problems to which Hydrology provides answers. 3) Methodological approach to hydrological sciences. 4) Water balance and the hydrological cycle. 5) Hydrological processes overview. 6) Hydrological data and
Understanding Hydrological Processes in an Ungauged Catchment in sub-Saharan Africa. DISSERTATION. Submitted in fulfilment of the requirements of the Board for Doctorates of Delft University of Technology and of the Academic Board of the UNESCO-IHE Institute for Water Education for the Degree of DOCTOR.
hydrological processes in a set of small research catchments located in a middle mountain area, paying especial attention to the seasonal aspects. Although some modelling exercises have been undertaken (e.g. Llorens, 1997; Gallart et al. 2000;. Anderton et al., 2002a, b), only results and interpretations from observations
Scientific Investigations Report 2009–5126. National Water-Quality Assessment (NAWQA) Program. Identifying Hydrologic Processes in Agricultural Watersheds. Using Precipitation-Runoff Models. Saturation excess runoff. Infiltration excess runoff. Unsaturated lateral preferential flow. Saturated lateral preferential flow.
28 Aug 2007 Performance of process-based hydrological models is usually assessed through comparison between simulated and measured streamflow. Although necessary, this analysis is not sufficient to estimate the quality and realism of the modelling since streamflow integrates all processes of the water cycle,
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