A simple procedure to model water level fluctuations in partially inundated wetlands

J F M Spieksma; J M Schouwenaars

doi:10.1016/S0022-1694(96)03271-4

A simple procedure to model water level fluctuations in partially inundated wetlands

J F M Spieksma^*
, J M Schouwenaars

^*Corresponding author for this work

Research output: Contribution to journal › Article › Academic › peer-review

10 Citations (Scopus)

Abstract

When modelling groundwater behaviour in wetlands, there are specific problems related to the presence of open water in small-sized mosaic patterns. A simple quasi two-dimensional model to predict water level fluctuations in partially inundated wetlands is presented. In this model, the ratio between inundated and non-inundated areas provides an adequate description of water storage properties. This concept can be implemented in any hydrological model. Two examples of such an implementation in the soil water flow model SWATRE are presented in this paper. (C) 1997 Elsevier Science B.V.

Original language	English
Pages (from-to)	324-335
Number of pages	12
Journal	Journal of Hydrology
Volume	196
Issue number	1-4
DOIs	https://doi.org/10.1016/S0022-1694(96)03271-4
Publication status	Published - Sept-1997

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A simple procedure to model water level fluctuations in partially inundated wetlands
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abstract = "When modelling groundwater behaviour in wetlands, there are specific problems related to the presence of open water in small-sized mosaic patterns. A simple quasi two-dimensional model to predict water level fluctuations in partially inundated wetlands is presented. In this model, the ratio between inundated and non-inundated areas provides an adequate description of water storage properties. This concept can be implemented in any hydrological model. Two examples of such an implementation in the soil water flow model SWATRE are presented in this paper. (C) 1997 Elsevier Science B.V.",

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N2 - When modelling groundwater behaviour in wetlands, there are specific problems related to the presence of open water in small-sized mosaic patterns. A simple quasi two-dimensional model to predict water level fluctuations in partially inundated wetlands is presented. In this model, the ratio between inundated and non-inundated areas provides an adequate description of water storage properties. This concept can be implemented in any hydrological model. Two examples of such an implementation in the soil water flow model SWATRE are presented in this paper. (C) 1997 Elsevier Science B.V.

AB - When modelling groundwater behaviour in wetlands, there are specific problems related to the presence of open water in small-sized mosaic patterns. A simple quasi two-dimensional model to predict water level fluctuations in partially inundated wetlands is presented. In this model, the ratio between inundated and non-inundated areas provides an adequate description of water storage properties. This concept can be implemented in any hydrological model. Two examples of such an implementation in the soil water flow model SWATRE are presented in this paper. (C) 1997 Elsevier Science B.V.

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U2 - 10.1016/S0022-1694(96)03271-4

DO - 10.1016/S0022-1694(96)03271-4

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EP - 335

JO - Journal of Hydrology

JF - Journal of Hydrology

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ER -

A simple procedure to model water level fluctuations in partially inundated wetlands

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