Karagiannis, G. and Hou, Z. and Huang, M. and Lin, G. (2022) 'Inverse Modeling of Hydrologic Parameters in CLM4 via Generalized Polynomial Chaos in the Bayesian Framework.', Computation, 10 (5). p. 72.
Abstract
In this work, generalized polynomial chaos (gPC) expansion for land surface model parameter estimation is evaluated. We perform inverse modeling and compute the posterior distribution of the critical hydrological parameters that are subject to great uncertainty in the Community Land Model (CLM) for a given value of the output LH. The unknown parameters include those that have been identified as the most influential factors on the simulations of surface and subsurface runoff, latent and sensible heat fluxes, and soil moisture in CLM4.0. We set up the inversion problem in the Bayesian framework in two steps: (i) building a surrogate model expressing the input–output mapping, and (ii) performing inverse modeling and computing the posterior distributions of the input parameters using observation data for a given value of the output LH. The development of the surrogate model is carried out with a Bayesian procedure based on the variable selection methods that use gPC expansions. Our approach accounts for bases selection uncertainty and quantifies the importance of the gPC terms, and, hence, all of the input parameters, via the associated posterior probabilities.
Item Type: | Article |
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Full text: | (VoR) Version of Record Available under License - Creative Commons Attribution 4.0. Download PDF (1853Kb) |
Status: | Peer-reviewed |
Publisher Web site: | https://doi.org/10.3390/computation10050072 |
Publisher statement: | © 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/ 4.0/). |
Date accepted: | 29 April 2022 |
Date deposited: | 20 May 2022 |
Date of first online publication: | 05 May 2022 |
Date first made open access: | 20 May 2022 |
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