TY - JOUR
T1 - Polynomial chaos quadrature-based minimum variance approach for source parameters estimation
AU - Madankan, R.
AU - Singla, P.
AU - Patra, A.
AU - Bursik, M.
AU - Dehn, J.
AU - Jones, M.
AU - Pavolonis, M.
AU - Pitman, B.
AU - Singh, T.
AU - Webley, P.
N1 - Funding Information:
This material is based upon work supported by the National Science Foundation under Awards No. 1054759 and CMMI-1131074.
PY - 2012
Y1 - 2012
N2 - We present a polynomial chaos based minimum variance formulation to solve inverse problems. The utility of the proposed approach is evaluated by considering the ash transport problem arising due to volcanic eruption. Volcanic ash advisory centers generally makes use of mathematical models for column eruption and advection and diffusion of ash cloud in atmosphere. These models require input data on source conditions such as vent radius, vent velocity and distribution of ash-particle size. The inputs are usually not well constrained, and estimates of the uncertainty in the inputs is needed to make accurate predictions of cloud motion. The recent eruption of Eyjafjallajökull, Iceland in April 2010 is considered as test example. For validation, the puff advection and diffusion model is used to hindcast the motion of the ash cloud through time concentrating on the period 14-16 April 2010. Variability in the height and loading of the eruption is introduced through the volcano column model bent. Output uncertainty due to uncertain input parameters is determined with a polynomial chaos quadrature (PCQ)-based sampling of the multidimensional puff input vector space. Furthermore, the posterior distribution for input parameters is obtained by assimilating satellite imagery data with PCQ predictions using a minimum variance approach.
AB - We present a polynomial chaos based minimum variance formulation to solve inverse problems. The utility of the proposed approach is evaluated by considering the ash transport problem arising due to volcanic eruption. Volcanic ash advisory centers generally makes use of mathematical models for column eruption and advection and diffusion of ash cloud in atmosphere. These models require input data on source conditions such as vent radius, vent velocity and distribution of ash-particle size. The inputs are usually not well constrained, and estimates of the uncertainty in the inputs is needed to make accurate predictions of cloud motion. The recent eruption of Eyjafjallajökull, Iceland in April 2010 is considered as test example. For validation, the puff advection and diffusion model is used to hindcast the motion of the ash cloud through time concentrating on the period 14-16 April 2010. Variability in the height and loading of the eruption is introduced through the volcano column model bent. Output uncertainty due to uncertain input parameters is determined with a polynomial chaos quadrature (PCQ)-based sampling of the multidimensional puff input vector space. Furthermore, the posterior distribution for input parameters is obtained by assimilating satellite imagery data with PCQ predictions using a minimum variance approach.
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U2 - 10.1016/j.procs.2012.04.122
DO - 10.1016/j.procs.2012.04.122
M3 - Conference article
AN - SCOPUS:84878534149
SN - 1877-0509
VL - 9
SP - 1129
EP - 1138
JO - Procedia Computer Science
JF - Procedia Computer Science
T2 - 12th Annual International Conference on Computational Science, ICCS 2012
Y2 - 4 June 2012 through 6 June 2012
ER -