Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding

Distributed catchment models are widely used tools for predicting hydrologic behavior. While distributed models require many parameters to describe a system, they are expected to simulate behavior that is more consistent with observed processes. However, obtaining a single set of acceptable para...

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Main Authors: C. Kelleher, B. McGlynn, T. Wagener
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/21/3325/2017/hess-21-3325-2017.pdf
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spelling doaj-9720630589d04c19820c3c885c1447e22020-11-24T22:58:54ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-07-01213325335210.5194/hess-21-3325-2017Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understandingC. Kelleher0C. Kelleher1B. McGlynn2T. Wagener3T. Wagener4Department of Earth Sciences, Syracuse University, Syracuse, NY, 13244, USADepartment of Earth and Ocean Sciences, Nicholas School of the Environment, Duke University, Durham, NC, 27706, USADepartment of Earth and Ocean Sciences, Nicholas School of the Environment, Duke University, Durham, NC, 27706, USADepartment of Civil Engineering, University of Bristol, Bristol, BS8 1TR, UKCabot Institute, University of Bristol, Bristol, BS8 1TR, UKDistributed catchment models are widely used tools for predicting hydrologic behavior. While distributed models require many parameters to describe a system, they are expected to simulate behavior that is more consistent with observed processes. However, obtaining a single set of acceptable parameters can be problematic, as parameter equifinality often results in several <q>behavioral</q> sets that fit observations (typically streamflow). In this study, we investigate the extent to which equifinality impacts a typical distributed modeling application. We outline a hierarchical approach to reduce the number of behavioral sets based on regional, observation-driven, and expert-knowledge-based constraints. For our application, we explore how each of these constraint classes reduced the number of <q>behavioral</q> parameter sets and altered distributions of spatiotemporal simulations, simulating a well-studied headwater catchment, Stringer Creek, Montana, using the distributed hydrology–soil–vegetation model (DHSVM). As a demonstrative exercise, we investigated model performance across 10 000 parameter sets. Constraints on regional signatures, the hydrograph, and two internal measurements of snow water equivalent time series reduced the number of behavioral parameter sets but still left a small number with similar goodness of fit. This subset was ultimately further reduced by incorporating pattern expectations of groundwater table depth across the catchment. Our results suggest that utilizing a hierarchical approach based on regional datasets, observations, and expert knowledge to identify behavioral parameter sets can reduce equifinality and bolster more careful application and simulation of spatiotemporal processes via distributed modeling at the catchment scale.https://www.hydrol-earth-syst-sci.net/21/3325/2017/hess-21-3325-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Kelleher
C. Kelleher
B. McGlynn
T. Wagener
T. Wagener
spellingShingle C. Kelleher
C. Kelleher
B. McGlynn
T. Wagener
T. Wagener
Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
Hydrology and Earth System Sciences
author_facet C. Kelleher
C. Kelleher
B. McGlynn
T. Wagener
T. Wagener
author_sort C. Kelleher
title Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
title_short Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
title_full Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
title_fullStr Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
title_full_unstemmed Characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
title_sort characterizing and reducing equifinality by constraining a distributed catchment model with regional signatures, local observations, and process understanding
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-07-01
description Distributed catchment models are widely used tools for predicting hydrologic behavior. While distributed models require many parameters to describe a system, they are expected to simulate behavior that is more consistent with observed processes. However, obtaining a single set of acceptable parameters can be problematic, as parameter equifinality often results in several <q>behavioral</q> sets that fit observations (typically streamflow). In this study, we investigate the extent to which equifinality impacts a typical distributed modeling application. We outline a hierarchical approach to reduce the number of behavioral sets based on regional, observation-driven, and expert-knowledge-based constraints. For our application, we explore how each of these constraint classes reduced the number of <q>behavioral</q> parameter sets and altered distributions of spatiotemporal simulations, simulating a well-studied headwater catchment, Stringer Creek, Montana, using the distributed hydrology–soil–vegetation model (DHSVM). As a demonstrative exercise, we investigated model performance across 10 000 parameter sets. Constraints on regional signatures, the hydrograph, and two internal measurements of snow water equivalent time series reduced the number of behavioral parameter sets but still left a small number with similar goodness of fit. This subset was ultimately further reduced by incorporating pattern expectations of groundwater table depth across the catchment. Our results suggest that utilizing a hierarchical approach based on regional datasets, observations, and expert knowledge to identify behavioral parameter sets can reduce equifinality and bolster more careful application and simulation of spatiotemporal processes via distributed modeling at the catchment scale.
url https://www.hydrol-earth-syst-sci.net/21/3325/2017/hess-21-3325-2017.pdf
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