Matches in SemOpenAlex for { <https://semopenalex.org/work/W170909306> ?p ?o ?g. }
Showing items 1 to 93 of
93
with 100 items per page.
- W170909306 endingPage "56" @default.
- W170909306 startingPage "39" @default.
- W170909306 abstract "The detailed model presented is a development of an exponential store model (TOPMODEL) previously described (Beven and Kirkby, 1979). The continuity equation for saturated sub-surface flow is expressed in terms of unit runoff which emphasizes the relatively low spatial variation in rates. For this reason kinematic wave solutions have not been used to solve the partial differential equation. A single unsaturated and a saturated store are considered at each point down the hillslope length, the former delaying infiltration and the latter providing downslope sub-surface flow and establishing saturated contributing areas.The total sub-surface flow at saturation, slope gradient and hillslope plan form are used to generate flow differences down the length of the hillslope profile. Simulations show the generation of saturated overland flow at downslope sites where flow converges, superimposed on a hydrograph which is largely controlled by the convex (in profile) divide area. This suggests that for most natural slopes, the runoff delivered to channel banks may be estimated efficiently from two separate linked component models. The first forecasts spatially uniform flow at rates determined by topography and soils in the hilltop divide areas. This model is able to forecast the changing saturated area on which the second component model forecasts the saturated overland flow. This or another appropriate hillslope flow model may be combined with a flow routing algorithm for the channel network to give catchment hydrological response. In simple cases of spatially constant network routing velocity, the resulting combined model is identical to the Geomorphological Unit Hydrograph of Rodríguez-Iturbe, providing an explicit physical meaning for his theoretical unit response functions as the hillslope base unit hydrograph." @default.
- W170909306 created "2016-06-24" @default.
- W170909306 creator A5063594028 @default.
- W170909306 date "1986-01-01" @default.
- W170909306 modified "2023-10-11" @default.
- W170909306 title "A Runoff Simulation Model Based on Hillslope Topography" @default.
- W170909306 cites W138011209 @default.
- W170909306 cites W1979393148 @default.
- W170909306 cites W1980688843 @default.
- W170909306 cites W1981646498 @default.
- W170909306 cites W2032874589 @default.
- W170909306 cites W2047692953 @default.
- W170909306 cites W2083783942 @default.
- W170909306 cites W2091815988 @default.
- W170909306 cites W3033884623 @default.
- W170909306 doi "https://doi.org/10.1007/978-94-009-4678-1_3" @default.
- W170909306 hasPublicationYear "1986" @default.
- W170909306 type Work @default.
- W170909306 sameAs 170909306 @default.
- W170909306 citedByCount "23" @default.
- W170909306 countsByYear W1709093062013 @default.
- W170909306 countsByYear W1709093062014 @default.
- W170909306 countsByYear W1709093062021 @default.
- W170909306 countsByYear W1709093062023 @default.
- W170909306 crossrefType "book-chapter" @default.
- W170909306 hasAuthorship W170909306A5063594028 @default.
- W170909306 hasConcept C103272765 @default.
- W170909306 hasConcept C114614502 @default.
- W170909306 hasConcept C114793014 @default.
- W170909306 hasConcept C127313418 @default.
- W170909306 hasConcept C153294291 @default.
- W170909306 hasConcept C153400128 @default.
- W170909306 hasConcept C154936535 @default.
- W170909306 hasConcept C159390177 @default.
- W170909306 hasConcept C159750122 @default.
- W170909306 hasConcept C187320778 @default.
- W170909306 hasConcept C18903297 @default.
- W170909306 hasConcept C205649164 @default.
- W170909306 hasConcept C2524010 @default.
- W170909306 hasConcept C2779313249 @default.
- W170909306 hasConcept C31258907 @default.
- W170909306 hasConcept C33923547 @default.
- W170909306 hasConcept C38349280 @default.
- W170909306 hasConcept C41008148 @default.
- W170909306 hasConcept C43978264 @default.
- W170909306 hasConcept C50477045 @default.
- W170909306 hasConcept C74172769 @default.
- W170909306 hasConcept C76886044 @default.
- W170909306 hasConcept C86803240 @default.
- W170909306 hasConcept C9930424 @default.
- W170909306 hasConceptScore W170909306C103272765 @default.
- W170909306 hasConceptScore W170909306C114614502 @default.
- W170909306 hasConceptScore W170909306C114793014 @default.
- W170909306 hasConceptScore W170909306C127313418 @default.
- W170909306 hasConceptScore W170909306C153294291 @default.
- W170909306 hasConceptScore W170909306C153400128 @default.
- W170909306 hasConceptScore W170909306C154936535 @default.
- W170909306 hasConceptScore W170909306C159390177 @default.
- W170909306 hasConceptScore W170909306C159750122 @default.
- W170909306 hasConceptScore W170909306C187320778 @default.
- W170909306 hasConceptScore W170909306C18903297 @default.
- W170909306 hasConceptScore W170909306C205649164 @default.
- W170909306 hasConceptScore W170909306C2524010 @default.
- W170909306 hasConceptScore W170909306C2779313249 @default.
- W170909306 hasConceptScore W170909306C31258907 @default.
- W170909306 hasConceptScore W170909306C33923547 @default.
- W170909306 hasConceptScore W170909306C38349280 @default.
- W170909306 hasConceptScore W170909306C41008148 @default.
- W170909306 hasConceptScore W170909306C43978264 @default.
- W170909306 hasConceptScore W170909306C50477045 @default.
- W170909306 hasConceptScore W170909306C74172769 @default.
- W170909306 hasConceptScore W170909306C76886044 @default.
- W170909306 hasConceptScore W170909306C86803240 @default.
- W170909306 hasConceptScore W170909306C9930424 @default.
- W170909306 hasLocation W1709093061 @default.
- W170909306 hasOpenAccess W170909306 @default.
- W170909306 hasPrimaryLocation W1709093061 @default.
- W170909306 hasRelatedWork W1966190258 @default.
- W170909306 hasRelatedWork W1985787922 @default.
- W170909306 hasRelatedWork W1999630887 @default.
- W170909306 hasRelatedWork W2038212370 @default.
- W170909306 hasRelatedWork W2052495673 @default.
- W170909306 hasRelatedWork W2078571788 @default.
- W170909306 hasRelatedWork W2095334919 @default.
- W170909306 hasRelatedWork W2133684869 @default.
- W170909306 hasRelatedWork W2355860219 @default.
- W170909306 hasRelatedWork W377649474 @default.
- W170909306 isParatext "false" @default.
- W170909306 isRetracted "false" @default.
- W170909306 magId "170909306" @default.
- W170909306 workType "book-chapter" @default.