TL;DR: The European Soil Erosion Model (EUROSEM) as mentioned in this paper is a dynamic distributed model able to simulate sediment transport, erosion and deposition over the land surface by rill and interill processes in single storms for both individual fields and small catchments.
TL;DR: In this article, a unified synthesis of the hydrologic response of a catchment to surface runoff is attempted by linking the instantaneous unit hydrograph (IUH) with the geomorphologic parameters of a basin.
Abstract: A unifying synthesis of the hydrologic response of a catchment to surface runoff is attempted by linking the instantaneous unit hydrograph (IUH) with the geomorphologic parameters of a basin. Equations of general character are derived which express the IUH as a function of Horton's numbers RA, RB, and RL; an internal scale parameter LΩ and a mean velocity of streamflow v. The IUH is time varying in character both throughout the storm and for different storms. This variability is accounted for by the variability in the mean streamflow velocity. The underlying unity in the nature of the geomorphologic structure is thus carried over to the great variety of hydrologic responses that occur in nature. An approach is initiated to the problem of hydrologic similarity.
TL;DR: The Xinanjiang model as discussed by the authors is a rainfall-runoff, distributed, basin model for use in humid and semi-humid regions, where evapotranspiration component is represented by a model of three soil layers.
TL;DR: In this paper, the authors present a survey of statistical methods in hydrology, including water yield and snowmelt runoff, water quality estimation, and water evaporation.
Abstract: 1. Introduction to Hydrology. 2. Statistical Methods in Hydrology. 3. Watershed Characteristics. 4. Precipitation. 5. Frequency Analysis. 6. Subsurface Hydrology. 7. Peak Discharge Estimation. 8. Hydrologic Design Methods. 9. Hydrograph Analysis and Synthesis. 10. Channel Routing. 11. Reservoir Routing. 12. Water Yield and Snowmelt Runoff. 13. Water Quality Estimation. 14. Evaporation. 15. Erosion and Sedimentation. References. Index.
TL;DR: Ashby et al. as discussed by the authors proposed a more general coupled model that incorporates a new two-dimensional overland flow simulator into the parallel three-dimensional variably saturated subsurface flow code ParFlow.