Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes

Lakes might be sentinels of climate change, but the uncertainty in their main feedback to the atmosphere – heat-exchange fluxes – is often not considered within climate models. Additionally, these fluxes are seldom measured, hindering critical evaluation of model output. Analysis of the Canadian...

Full description

Bibliographic Details
Main Authors: J.-L. Guerrero, P. Pernica, H. Wheater, M. Mackay, C. Spence
Format: Article
Language:English
Published: Copernicus Publications 2017-12-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/21/6345/2017/hess-21-6345-2017.pdf
id doaj-57bfd58f86f4489ea40558857707fe03
record_format Article
spelling doaj-57bfd58f86f4489ea40558857707fe032020-11-25T00:12:09ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-12-01216345636210.5194/hess-21-6345-2017Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemesJ.-L. Guerrero0J.-L. Guerrero1P. Pernica2H. Wheater3M. Mackay4C. Spence5Global Institute for Water Security, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, CanadaNorwegian Institute for Water Research, Gaustadalléen 21, 0349 Oslo, NorwayGlobal Institute for Water Security, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, CanadaGlobal Institute for Water Security, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, CanadaScience and Technology Branch, Environment and Climate Change Canada, 4905 Dufferin Str., Toronto, ON, M3H5T4, CanadaScience and Technology Branch, Environment and Climate Change Canada, 11 Innovation Boulevard, Saskatoon, SK, CanadaLakes might be sentinels of climate change, but the uncertainty in their main feedback to the atmosphere – heat-exchange fluxes – is often not considered within climate models. Additionally, these fluxes are seldom measured, hindering critical evaluation of model output. Analysis of the Canadian Small Lake Model (CSLM), a one-dimensional integral lake model, was performed to assess its ability to reproduce diurnal and seasonal variations in heat fluxes and the sensitivity of simulated fluxes to changes in model parameters, i.e., turbulent transport parameters and the light extinction coefficient (<i>K</i><sub>d</sub>). A C++ open-source software package, Problem Solving environment for Uncertainty Analysis and Design Exploration (PSUADE), was used to perform sensitivity analysis (SA) and identify the parameters that dominate model behavior. The generalized likelihood uncertainty estimation (GLUE) was applied to quantify the fluxes' uncertainty, comparing daily-averaged eddy-covariance observations to the output of CSLM. Seven qualitative and two quantitative SA methods were tested, and the posterior likelihoods of the modeled parameters, obtained from the GLUE analysis, were used to determine the dominant parameters and the uncertainty in the modeled fluxes. Despite the ubiquity of the equifinality issue – different parameter-value combinations yielding equivalent results – the answer to the question was unequivocal: <i>K</i><sub>d</sub>, a measure of how much light penetrates the lake, dominates sensible and latent heat fluxes, and the uncertainty in their estimates is strongly related to the accuracy with which <i>K</i><sub>d</sub> is determined. This is important since accurate and continuous measurements of <i>K</i><sub>d</sub> could reduce modeling uncertainty.https://www.hydrol-earth-syst-sci.net/21/6345/2017/hess-21-6345-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J.-L. Guerrero
J.-L. Guerrero
P. Pernica
H. Wheater
M. Mackay
C. Spence
spellingShingle J.-L. Guerrero
J.-L. Guerrero
P. Pernica
H. Wheater
M. Mackay
C. Spence
Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
Hydrology and Earth System Sciences
author_facet J.-L. Guerrero
J.-L. Guerrero
P. Pernica
H. Wheater
M. Mackay
C. Spence
author_sort J.-L. Guerrero
title Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
title_short Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
title_full Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
title_fullStr Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
title_full_unstemmed Parameter sensitivity analysis of a 1-D cold region lake model for land-surface schemes
title_sort parameter sensitivity analysis of a 1-d cold region lake model for land-surface schemes
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-12-01
description Lakes might be sentinels of climate change, but the uncertainty in their main feedback to the atmosphere – heat-exchange fluxes – is often not considered within climate models. Additionally, these fluxes are seldom measured, hindering critical evaluation of model output. Analysis of the Canadian Small Lake Model (CSLM), a one-dimensional integral lake model, was performed to assess its ability to reproduce diurnal and seasonal variations in heat fluxes and the sensitivity of simulated fluxes to changes in model parameters, i.e., turbulent transport parameters and the light extinction coefficient (<i>K</i><sub>d</sub>). A C++ open-source software package, Problem Solving environment for Uncertainty Analysis and Design Exploration (PSUADE), was used to perform sensitivity analysis (SA) and identify the parameters that dominate model behavior. The generalized likelihood uncertainty estimation (GLUE) was applied to quantify the fluxes' uncertainty, comparing daily-averaged eddy-covariance observations to the output of CSLM. Seven qualitative and two quantitative SA methods were tested, and the posterior likelihoods of the modeled parameters, obtained from the GLUE analysis, were used to determine the dominant parameters and the uncertainty in the modeled fluxes. Despite the ubiquity of the equifinality issue – different parameter-value combinations yielding equivalent results – the answer to the question was unequivocal: <i>K</i><sub>d</sub>, a measure of how much light penetrates the lake, dominates sensible and latent heat fluxes, and the uncertainty in their estimates is strongly related to the accuracy with which <i>K</i><sub>d</sub> is determined. This is important since accurate and continuous measurements of <i>K</i><sub>d</sub> could reduce modeling uncertainty.
url https://www.hydrol-earth-syst-sci.net/21/6345/2017/hess-21-6345-2017.pdf
work_keys_str_mv AT jlguerrero parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
AT jlguerrero parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
AT ppernica parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
AT hwheater parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
AT mmackay parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
AT cspence parametersensitivityanalysisofa1dcoldregionlakemodelforlandsurfaceschemes
_version_ 1725400918169485312