By Andreas Lang, Kirsten P. Hennrich, Richard Dikau
This quantity provides a suite of papers given at a Rhine-LUCIFS (Land use and weather effect on fluvial systems), the purpose being to collect researchers with longstanding adventure in constructing ideas and modelling techniques for long-term panorama evolution and scientists concerned about extra classical experiences at the evolution of the Rhine river approach. it really is divided into elements: half one stories the Rhine river process and offers case reviews to illustrate the kinds of knowledge that may be extracted from sedimentary data. half offers a state-of-the-art evaluate on strategies for fluvial procedure learn, in addition to modelling the elements of huge river basins, written through top ecu scientists during this field.
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Extra info for Long Term Hillslope and Fluvial System Modelling: Concepts and Case Studies from the Rhine River Catchment
Springer–Verlag, Berlin. 50 J. Wainwright et al. A. (1992): Physically based hydrologic modelling. 2. is the concept realistic? Water Resources Research 28: 2659–2666. J. (1974): Surface Wash at the Semi–Arid Break in Slope. Zeitschrift fr Geomorphologie, Supplementband 21: 151–76. Kotarba, A. (1980): Splash Transport in the Steppe Zone of Mongolia. Zeitschrift f¨ ur Geomorphologie, Supplementband 35: 92–102. B. (1958): Factors aﬀecting sediment delivery rates in the Red Hills physiographic area.
However, the implementation of the process structure within the model from the outset is still no guarantee of performance (Parsons and Wainwright, 2000). In essence, it is still necessary to follow a hybrid approach where ﬁeld and laboratory experiments are necessary to provide reﬁnements to the model structure and component interactions at the same time as the collection of parameterization data. , 1992). However, their structure has the disadvantage of propagating errors, for example in parameter measurement, through the prediction process.
Sidorchuk, A. (1999): Dynamic and static models of gully erosion. Catena, 37: 401–414. Linking Short– and Long–Term Soil–Erosion Modelling John Wainwright1 , Anthony J. Parsons2 , Katerina Michaelides3 , D. Mark Powell2 , and Richard Brazier1 1 Environmental Monitoring and Modelling Research Group, Department of Geography, King’s College London, Strand, London, WC2R 2LS, UK 2 Department of Geography, Leicester University, University Road, Leicester, LE1 7RH, UK 3 School of Geographical Sciences, Bristol University, University Road, Bristol, BS8 1SS, UK 1 Introduction Soil erosion by overland ﬂow is a signiﬁcant process over large areas of the Earth.
Long Term Hillslope and Fluvial System Modelling: Concepts and Case Studies from the Rhine River Catchment by Andreas Lang, Kirsten P. Hennrich, Richard Dikau