2013
DOI: 10.3390/e15062398
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On the Use of Information Theory to Quantify Parameter Uncertainty in Groundwater Modeling

Abstract: Abstract:We applied information theory to quantify parameter uncertainty in a groundwater flow model. A number of parameters in groundwater modeling are often used with lack of knowledge of site conditions due to heterogeneity of hydrogeologic properties and limited access to complex geologic structures. The present Information Theory-based (ITb) approach is to adopt entropy as a measure of uncertainty at the most probable state of hydrogeologic conditions. The most probable conditions are those at which the g… Show more

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Cited by 3 publications
(2 citation statements)
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“…A significant amount of work has been done on the issue of upscaling [8][9][10][11][12][13][14][15][16][17][18]. Hydrologists need ways to provide modeling properties at larger scales that appropriately represent the numerous smaller scale variations present in natural heterogeneous systems [16,[19][20][21][22][23]. While the work presented here is closely related to the scale-up problem, it does not directly extend previous work done in this area.…”
Section: Introductionmentioning
confidence: 99%
“…A significant amount of work has been done on the issue of upscaling [8][9][10][11][12][13][14][15][16][17][18]. Hydrologists need ways to provide modeling properties at larger scales that appropriately represent the numerous smaller scale variations present in natural heterogeneous systems [16,[19][20][21][22][23]. While the work presented here is closely related to the scale-up problem, it does not directly extend previous work done in this area.…”
Section: Introductionmentioning
confidence: 99%
“…The development and application of a groundwater model is a common practice for the management of groundwater resources [7]. Many scientific efforts have been made to develop more comprehensive and computationally efficient models involving complex hydrogeologic processes [8,9]. In many numerical models of a groundwater aquifer, for example, Feflow and MODFLOW, the continuous domain of groundwater system is replaced by a discretized grid network and the governing groundwater flow equation is solved at the network nodes.…”
Section: Introductionmentioning
confidence: 99%