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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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 |
work_keys_str_mv |
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