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Hydrologic data assimilation using particle Markov chain Monte Carlo simulation: Theory,concepts and applications
Institution:1. Department of Civil and Environmental Engineering, University of California, Irvine, USA;2. Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, The Netherlands;3. Biometris, Wageningen University and Research Centre, 6700 AC, Wageningen, The Netherlands;4. Center for Nonlinear Dynamics in Economics and Finance, University of Amsterdam, The Netherlands;5. Department of Water Management, Delft University of Technology, Delft, The Netherlands;1. State Key Laboratory of Lake Science and Environment, Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 East Beijing Road, Nanjing 210008, China;2. Department of Aquatic Ecosystem Analysis and Management, Helmholtz Centre for Environmental Research-UFZ, D-39114 Magdeburg, Germany;3. Department of Bioenergy, Helmholtz Centre for Environmental Research-UFZ, D-39114 Magdeburg, Germany;4. Department of Hydrology, Water Management and Water Protection, Leichtweiss Institute for Hydraulics and Water Resources, University of Braunschweig, D-38106 Braunschweig, Germany
Abstract:During the past decades much progress has been made in the development of computer based methods for parameter and predictive uncertainty estimation of hydrologic models. The goal of this paper is twofold. As part of this special anniversary issue we first shortly review the most important historical developments in hydrologic model calibration and uncertainty analysis that has led to current perspectives. Then, we introduce theory, concepts and simulation results of a novel data assimilation scheme for joint inference of model parameters and state variables. This Particle-DREAM method combines the strengths of sequential Monte Carlo sampling and Markov chain Monte Carlo simulation and is especially designed for treatment of forcing, parameter, model structural and calibration data error. Two different variants of Particle-DREAM are presented to satisfy assumptions regarding the temporal behavior of the model parameters. Simulation results using a 40-dimensional atmospheric “toy” model, the Lorenz attractor and a rainfall–runoff model show that Particle-DREAM, P-DREAM(VP) and P-DREAM(IP) require far fewer particles than current state-of-the-art filters to closely track the evolving target distribution of interest, and provide important insights into the information content of discharge data and non-stationarity of model parameters. Our development follows formal Bayes, yet Particle-DREAM and its variants readily accommodate hydrologic signatures, informal likelihood functions or other (in)sufficient statistics if those better represent the salient features of the calibration data and simulation model used.
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