Journal Title
Title of Journal: J Earth Syst Sci
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Abbravation: Journal of Earth System Science
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Authors: Diego Rivera Yessica Rivas Alex Godoy
Publish Date: 2015/02/10
Volume: 124, Issue: 1, Pages: 49-59
Abstract
Hydrological models are simplified representations of natural processes and subject to errors Uncertainty bounds are a commonly used way to assess the impact of an input or model architecture uncertainty in model outputs Different sets of parameters could have equally robust goodnessoffit indicators which is known as Equifinality We assessed the outputs from a lumped conceptual hydrological model to an agricultural watershed in central Chile under strong interannual variability coefficient of variability of 25 by using the Equifinality concept and uncertainty bounds The simulation period ran from January 1999 to December 2006 Equifinality and uncertainty bounds from GLUE methodology Generalized Likelihood Uncertainty Estimation were used to identify parameter sets as potential representations of the system The aim of this paper is to exploit the use of uncertainty bounds to differentiate behavioural parameter sets in a simple hydrological model Then we analyze the presence of equifinality in order to improve the identification of relevant hydrological processes The water balance model for Chillan River exhibits at a first stage equifinality However it was possible to narrow the range for the parameters and eventually identify a set of parameters representing the behaviour of the watershed a behavioural model in agreement with observational and soft data calculation of areal precipitation over the watershed using an isohyetal map The mean width of the uncertainty bound around the predicted runoff for the simulation period decreased from 50 to 20 m3s−1 after fixing the parameter controlling the areal precipitation over the watershed This decrement is equivalent to decreasing the ratio between simulated and observed discharge from 52 to 25 Despite the criticisms against the GLUE methodology such as the lack of statistical formality it is identified as a useful tool assisting the modeller with the identification of critical parametersThe BFA model was coded in MATLAB by Dr© FulvioRivano and Leonardo Vega Codes and datasets are available on request This research was benefited from FONDECYT Grant Nos 11090032 and 1110298 We thank Dr Claire Baffaut and Dr José Luis Arumí for their comments and suggestions Thanks to Roto Quezada
Keywords:
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Other Papers In This Journal:
- Characterization of the atmospheric boundary layer from radiosonde observations along eastern end of monsoon trough of India
- Comparison of CloudSat and TRMM radar reflectivities
- Hydrologic modelling of the effect of snowmelt and temperature on a mountainous watershed
- Influence of soil moisture content on surface albedo and soil thermal parameters at a tropical station
- Evaluation of soft sediment deformation structures along the Fethiye–Burdur Fault Zone, SW Turkey
- Equatorial wave activity during 2007 over Gadanki, a tropical station
- Existence of torsional surface waves in an earth’s crustal layer lying over a sandy mantle
- Evaluation of precipitation and river discharge variations over southwestern Iran during recent decades
- Seasonal forecasting of tropical cyclogenesis over the North Indian Ocean
- Migration of the Ganga river and its implication on hydro-geological potential of Varanasi area, U.P., India
- Endemism due to climate change: Evidence from Poeciloneuron Bedd. (Clusiaceae) leaf fossil from Assam, India
- Study of vertical wind profiles in an urban area with complex terrain (Tehran)
- Efficient two-dimensional magnetotellurics modelling using implicitly restarted Lanczos method
- A comparative study for the estimation of geodetic point velocity by artificial neural networks
- Dust storm detection using random forests and physical-based approaches over the Middle East
- Ichnofabric analysis of the Tithonian shallow marine sediments (Bhadasar Formation) Jaisalmer Basin, India
- Effect of some climatic parameters on tropospheric and total ozone column over Alipore ( 22.52 ∘ N, 88.33 ∘ E), India
- Activity of radon ( 222 Rn) in the lower atmospheric surface layer of a typical rural site in south India
- Anthropogenic and impact spherules: Morphological similarity and chemical distinction – A case study from India and its implications
- Anthropogenic and impact spherules: Morphological similarity and chemical distinction – A case study from India and its implications
- Influence of rigid boundary on the propagation of torsional surface wave in an inhomogeneous layer
- Evidence of Late Quaternary seismicity from Yunam Tso, Lahaul and Spiti, NW Himalaya, India
- Century scale climate change in the central highlands of Sri Lanka
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