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...
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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 |
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