<i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"

Heterogeneity and complexity of hydrological processes offer substantial challenges to the hydrological modeller. Some hydrologists try to tackle this problem by introducing more and more detail in their models, or by setting-up more and more complicated models starting from basic principles at the...

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Main Author: H. H. G. Savenije
Format: Article
Language:English
Published: Copernicus Publications 2010-12-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/14/2681/2010/hess-14-2681-2010.pdf
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spelling doaj-3d2bfa7b06664aba9d537f173d96d8e82020-11-25T00:09:30ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382010-12-0114122681269210.5194/hess-14-2681-2010<i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"H. H. G. SavenijeHeterogeneity and complexity of hydrological processes offer substantial challenges to the hydrological modeller. Some hydrologists try to tackle this problem by introducing more and more detail in their models, or by setting-up more and more complicated models starting from basic principles at the smallest possible level. As we know, this reductionist approach leads to ever higher levels of equifinality and predictive uncertainty. On the other hand, simple, lumped and parsimonious models may be too simple to be realistic or representative of the dominant hydrological processes. In this commentary, a new approach is proposed that tries to find the middle way between complex distributed and simple lumped modelling approaches. Here we try to find the right level of simplification while avoiding over-simplification. Paraphrasing Einstein, the maxim is: make a model as simple as possible, but not simpler than that. The approach presented is process based, but not physically based in the traditional sense. Instead, it is based on a conceptual representation of the dominant physical processes in certain key elements of the landscape. The essence of the approach is that the model structure is made dependent on a limited number of landscape classes in which the topography is the main driver, but which can include geological, geomorphological or land-use classification. These classes are then represented by lumped conceptual models that act in parallel. The advantage of this approach over a fully distributed conceptualisation is that it retains maximum simplicity while taking into account observable landscape characteristics. http://www.hydrol-earth-syst-sci.net/14/2681/2010/hess-14-2681-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. H. G. Savenije
spellingShingle H. H. G. Savenije
<i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
Hydrology and Earth System Sciences
author_facet H. H. G. Savenije
author_sort H. H. G. Savenije
title <i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
title_short <i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
title_full <i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
title_fullStr <i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
title_full_unstemmed <i>HESS Opinions</i> "Topography driven conceptual modelling (FLEX-Topo)"
title_sort <i>hess opinions</i> "topography driven conceptual modelling (flex-topo)"
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2010-12-01
description Heterogeneity and complexity of hydrological processes offer substantial challenges to the hydrological modeller. Some hydrologists try to tackle this problem by introducing more and more detail in their models, or by setting-up more and more complicated models starting from basic principles at the smallest possible level. As we know, this reductionist approach leads to ever higher levels of equifinality and predictive uncertainty. On the other hand, simple, lumped and parsimonious models may be too simple to be realistic or representative of the dominant hydrological processes. In this commentary, a new approach is proposed that tries to find the middle way between complex distributed and simple lumped modelling approaches. Here we try to find the right level of simplification while avoiding over-simplification. Paraphrasing Einstein, the maxim is: make a model as simple as possible, but not simpler than that. The approach presented is process based, but not physically based in the traditional sense. Instead, it is based on a conceptual representation of the dominant physical processes in certain key elements of the landscape. The essence of the approach is that the model structure is made dependent on a limited number of landscape classes in which the topography is the main driver, but which can include geological, geomorphological or land-use classification. These classes are then represented by lumped conceptual models that act in parallel. The advantage of this approach over a fully distributed conceptualisation is that it retains maximum simplicity while taking into account observable landscape characteristics.
url http://www.hydrol-earth-syst-sci.net/14/2681/2010/hess-14-2681-2010.pdf
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