Titlebook: Distributed Hydrological Modelling; Michael B. Abbott,Jens Christian Refsgaard Book 1996 Kluwer Academic Publishers 1996 Erosion.GIS.Geoin

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Other International Organizations—ogy Distributed Model (IHDM, see Beven et al. 1987; Calver, 1988; Calver and Wood, 1995). These models claim to be physically-based (in accordance with the outline laid down by Freeze and Harlan, 1969) and to have parameters that are physically measurable in the field, at least in principle.

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Book 1996oughts, and indeed of everything else that has ever been recorded or remembered, and then to apply to this everything that is known about meteorology, plant physiology, soil physics, hydrogeology, sediment transport and everything else that is relevant within this context. Of course, no matter how m

Schlemms-Canal

Use Of GIS And Database with Distributed Modelling,the model in a stochastic context (Te Stroet, 1995). When many scenario’s have to be evaluated against each other, this becomes essential because a quantification of minimum and maximum effects prevents the hydrologist from making the wrong choices based on an erroneous model. Nowadays, the pure num

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,Comment on ’A Discussion of Distributed Hydrological Modelling’ by K. Beven,el validation as the validation of a site-specific model, while code verification refers to the testing of algorithms etc. Our terminology is defined and discussed in more details in this book by Refsgaard (Chapter 2) and Refsgaard and Storm (Chapter 3).

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0921-092X teorology, plant physiology, soil physics, hydrogeology, sediment transport and everything else that is relevant within this context. Of course, no matter how m978-94-010-6599-3978-94-009-0257-2Series ISSN 0921-092X Series E-ISSN 1872-4663

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耐寒

Distributed Physically-Based Modelling Of The Entire Land Phase of The Hydrological Cycle, namely that in order to obtain a useful outcome of the modelling exercise, variations in state-variables over space and time need to be considered and realistic representations of internal flow processes have to. be computed.