Runoff (surface flow) is one of the most important hydrological variable in supporting the activities of water resources development. A reliable prediction method to calculate the amount and rate of runoff from the land surface caused by the rain that falls in a watershed that is not equipped ...
Abramopoulos F, Rosenzweig C, Choudhuri B (1988) Improved ground hydrology calculations for global climate models (GCMs): soil water movement and evapotranspiration. J Clim 1:921–941 Google Scholar Albrecht F (1965) Untersuchungen des Wärme- und Wasserhaushalts der südlichen Kontinente. Ber...
Most ice sheet mass balance models make use of meltwater retention parameterizations to determine the runoff limit, but the runoff limit has never been directly measured. Lateral routing of meltwater is important for runoff calculations because any melt produced at the surface must be able to ...
Calculations of river- runoff in the GISS GCM: impact of a new land-surface parameterization and runoff routing model on the hydrology of the Amazon river. Clim. Dyn. 10, 349-361.Marengo J.A., Miller J.A., Russell G., Rosenzweig C., and Abramopoulos F. (1994), Calculations of ...
5 shows total concentration levels in the same order of magnitude in atmospheric deposition, river water, stormwater and treated wastewater, with highest total concentration in stormwater runoff, followed by atmospheric deposition. Concentrations in groundwater were not quantitatively measured above the LOQ...
As a result, surface waters, as receiving ecosystems, are at risk of being exposed to many of these chemicals, their byproducts and transformation products via point sources (e.g. waste water outlets) or diffuse sources (e.g. farmland runoff and drainage) (Stone et al., 2014, Stone et ...
calculations, making use of an antecedent precipitation index. For hydrograph separation, a wide range of filter parameters suited to urban environments were explored. Two approaches were then used to estimate groundwater recharge: (1) an empirical water balance using the surface runoff estimates as ...
Environmental transitions often result in resource mixtures that overcome limitations to microbial metabolism, resulting in biogeochemical hotspots and moments. Riverine systems, where groundwater mixes with surface water (the hyporheic zone), are spatia
Low salinity surface waters, called Modified Atlantic Water (MAW), enter in the Mediterranean Sea from the Strait of Gibraltar and occupy the first 0–100 m of the water column which overlies the outflowing saltier Levantine Intermediate Water (LIW) formed in the Levantine basin29. The MAW...
Scientists and practitioners agree that integrated water resource management is necessary, with an increasing need for research at the regional scale (103