Identifying the connective strength between model parameters and performance criteria

In hydrological models, parameters are used to represent the time-invariant characteristics of catchments and to capture different aspects of hydrological response. Hence, model parameters need to be identified based on their role in controlling the hydrological behaviour. For the identification...

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Main Authors: B. Guse, M. Pfannerstill, A. Gafurov, J. Kiesel, C. Lehr, N. Fohrer
Format: Article
Language:English
Published: Copernicus Publications 2017-11-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/21/5663/2017/hess-21-5663-2017.pdf
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author B. Guse
B. Guse
M. Pfannerstill
A. Gafurov
J. Kiesel
J. Kiesel
C. Lehr
C. Lehr
N. Fohrer
spellingShingle B. Guse
B. Guse
M. Pfannerstill
A. Gafurov
J. Kiesel
J. Kiesel
C. Lehr
C. Lehr
N. Fohrer
Identifying the connective strength between model parameters and performance criteria
Hydrology and Earth System Sciences
author_facet B. Guse
B. Guse
M. Pfannerstill
A. Gafurov
J. Kiesel
J. Kiesel
C. Lehr
C. Lehr
N. Fohrer
author_sort B. Guse
title Identifying the connective strength between model parameters and performance criteria
title_short Identifying the connective strength between model parameters and performance criteria
title_full Identifying the connective strength between model parameters and performance criteria
title_fullStr Identifying the connective strength between model parameters and performance criteria
title_full_unstemmed Identifying the connective strength between model parameters and performance criteria
title_sort identifying the connective strength between model parameters and performance criteria
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-11-01
description In hydrological models, parameters are used to represent the time-invariant characteristics of catchments and to capture different aspects of hydrological response. Hence, model parameters need to be identified based on their role in controlling the hydrological behaviour. For the identification of meaningful parameter values, multiple and complementary performance criteria are used that compare modelled and measured discharge time series. The reliability of the identification of hydrologically meaningful model parameter values depends on how distinctly a model parameter can be assigned to one of the performance criteria.<br><br> To investigate this, we introduce the new concept of connective strength between model parameters and performance criteria. The connective strength assesses the intensity in the interrelationship between model parameters and performance criteria in a bijective way. In our analysis of connective strength, model simulations are carried out based on a latin hypercube sampling. Ten performance criteria including Nash–Sutcliffe efficiency (NSE), Kling–Gupta efficiency (KGE) and its three components (alpha, beta and r) as well as RSR (the ratio of the root mean square error to the standard deviation) for different segments of the flow duration curve (FDC) are calculated.<br><br> With a joint analysis of two regression tree (RT) approaches, we derive how a model parameter is connected to different performance criteria. At first, RTs are constructed using each performance criterion as the target variable to detect the most relevant model parameters for each performance criterion. Secondly, RTs are constructed using each parameter as the target variable to detect which performance criteria are impacted by changes in the values of one distinct model parameter. Based on this, appropriate performance criteria are identified for each model parameter.<br><br> In this study, a high bijective connective strength between model parameters and performance criteria is found for low- and mid-flow conditions. Moreover, the RT analyses emphasise the benefit of an individual analysis of the three components of KGE and of the FDC segments. Furthermore, the RT analyses highlight under which conditions these performance criteria provide insights into precise parameter identification. Our results show that separate performance criteria are required to identify dominant parameters on low- and mid-flow conditions, whilst the number of required performance criteria for high flows increases with increasing process complexity in the catchment. Overall, the analysis of the connective strength between model parameters and performance criteria using RTs contribute to a more realistic handling of parameters and performance criteria in hydrological modelling.
url https://www.hydrol-earth-syst-sci.net/21/5663/2017/hess-21-5663-2017.pdf
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spelling doaj-2df958799c5143f38afeef600a64a6f22020-11-25T01:00:17ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-11-01215663567910.5194/hess-21-5663-2017Identifying the connective strength between model parameters and performance criteriaB. Guse0B. Guse1M. Pfannerstill2A. Gafurov3J. Kiesel4J. Kiesel5C. Lehr6C. Lehr7N. Fohrer8Christian Albrechts University of Kiel, Institute of Natural Resource Conservation, Department of Hydrology and Water Resources Management, Kiel, GermanyGFZ German Research Centre for Geosciences, Section 5.4 Hydrology, Potsdam, GermanyChristian Albrechts University of Kiel, Institute of Natural Resource Conservation, Department of Hydrology and Water Resources Management, Kiel, GermanyGFZ German Research Centre for Geosciences, Section 5.4 Hydrology, Potsdam, GermanyChristian Albrechts University of Kiel, Institute of Natural Resource Conservation, Department of Hydrology and Water Resources Management, Kiel, GermanyLeibniz Institute of Freshwater Ecology and Inland Fisheries (IGB), Berlin, GermanyLeibniz Centre for Agricultural Landscape Research (ZALF), Institute of Landscape Hydrology, Müncheberg, GermanyUniversity of Potsdam, Institute for Earth and Environmental Sciences, Potsdam, GermanyChristian Albrechts University of Kiel, Institute of Natural Resource Conservation, Department of Hydrology and Water Resources Management, Kiel, GermanyIn hydrological models, parameters are used to represent the time-invariant characteristics of catchments and to capture different aspects of hydrological response. Hence, model parameters need to be identified based on their role in controlling the hydrological behaviour. For the identification of meaningful parameter values, multiple and complementary performance criteria are used that compare modelled and measured discharge time series. The reliability of the identification of hydrologically meaningful model parameter values depends on how distinctly a model parameter can be assigned to one of the performance criteria.<br><br> To investigate this, we introduce the new concept of connective strength between model parameters and performance criteria. The connective strength assesses the intensity in the interrelationship between model parameters and performance criteria in a bijective way. In our analysis of connective strength, model simulations are carried out based on a latin hypercube sampling. Ten performance criteria including Nash–Sutcliffe efficiency (NSE), Kling–Gupta efficiency (KGE) and its three components (alpha, beta and r) as well as RSR (the ratio of the root mean square error to the standard deviation) for different segments of the flow duration curve (FDC) are calculated.<br><br> With a joint analysis of two regression tree (RT) approaches, we derive how a model parameter is connected to different performance criteria. At first, RTs are constructed using each performance criterion as the target variable to detect the most relevant model parameters for each performance criterion. Secondly, RTs are constructed using each parameter as the target variable to detect which performance criteria are impacted by changes in the values of one distinct model parameter. Based on this, appropriate performance criteria are identified for each model parameter.<br><br> In this study, a high bijective connective strength between model parameters and performance criteria is found for low- and mid-flow conditions. Moreover, the RT analyses emphasise the benefit of an individual analysis of the three components of KGE and of the FDC segments. Furthermore, the RT analyses highlight under which conditions these performance criteria provide insights into precise parameter identification. Our results show that separate performance criteria are required to identify dominant parameters on low- and mid-flow conditions, whilst the number of required performance criteria for high flows increases with increasing process complexity in the catchment. Overall, the analysis of the connective strength between model parameters and performance criteria using RTs contribute to a more realistic handling of parameters and performance criteria in hydrological modelling.https://www.hydrol-earth-syst-sci.net/21/5663/2017/hess-21-5663-2017.pdf