As observed by Hallema et al. (2016), the propagation of generated runoff depends on the ability of hillslope to retain and release water, which largely controls the hydrologic response over the course of a given rainfall event.
The hillslope's ability to retain and release water largely controls the hydrologic response over the course of a given rainfall event, and affects the propagation of generated runoff from the hillslope to the nearest channel in response to precipitation (Robinson and Sivapalan, 1996).
This study aims at separating contributions to streamflow originating from Presena and Presanella glaciers, both exerting a strong control on the hydrologic budget of the study site.
The hydrologic controls on the interaction between a shallow lake and a groundwater flow system have been determined for a coarse-textured landscape on the Boreal Plains of Canada.
Fluid transport properties of fault zones in the Nankai accretionary prism control static hydrologic behavior in the fault zone as well as dynamic fault processes.
The data collected make possible analyses of the hydrologic factors that control recovery and management of the groundwater-supply quality on Roi-Namur and on similar low-lying islands.
Model aggregation quickly eradicates curvature features and its spatial control on hydrologic patterns, while the level of coarsening possible in the hillslope still preserves vegetation patchiness.
It plays an important role in the hydrologic cycle, which controls groundwater potential.
Stormwater Control Measures (SCMs) have been developed to mitigate the hydrologic and water quality impacts of urban areas and IC.
