A Partitioned Kalman Filter and SmootherSource: Monthly Weather Review:;2002:;volume( 130 ):;issue: 005::page 1370Author:Fukumori, Ichiro
DOI: 10.1175/1520-0493(2002)130<1370:APKFAS>2.0.CO;2Publisher: American Meteorological Society
Abstract: A new approach is advanced for approximating Kalman filtering and smoothing suitable for oceanic and atmospheric data assimilation. The method solves the larger estimation problem by partitioning it into a series of smaller calculations. Errors with small correlation distances are derived by regional approximations, and errors associated with independent processes are evaluated separately from one another. The overall uncertainty of the model state, as well as the Kalman filter and smoother, is approximated by the sum of the corresponding individual components. The resulting smaller dimensionality of each separate element renders application of Kalman filtering and smoothing to the larger problem much more practical than otherwise. In particular, the approximation makes high-resolution global eddy-resolving data assimilation computationally viable. The approach is described and its efficacy demonstrated using a simple one-dimensional shallow water model.
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contributor author | Fukumori, Ichiro | |
date accessioned | 2017-06-09T16:14:22Z | |
date available | 2017-06-09T16:14:22Z | |
date copyright | 2002/05/01 | |
date issued | 2002 | |
identifier issn | 0027-0644 | |
identifier other | ams-63947.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4205006 | |
description abstract | A new approach is advanced for approximating Kalman filtering and smoothing suitable for oceanic and atmospheric data assimilation. The method solves the larger estimation problem by partitioning it into a series of smaller calculations. Errors with small correlation distances are derived by regional approximations, and errors associated with independent processes are evaluated separately from one another. The overall uncertainty of the model state, as well as the Kalman filter and smoother, is approximated by the sum of the corresponding individual components. The resulting smaller dimensionality of each separate element renders application of Kalman filtering and smoothing to the larger problem much more practical than otherwise. In particular, the approximation makes high-resolution global eddy-resolving data assimilation computationally viable. The approach is described and its efficacy demonstrated using a simple one-dimensional shallow water model. | |
publisher | American Meteorological Society | |
title | A Partitioned Kalman Filter and Smoother | |
type | Journal Paper | |
journal volume | 130 | |
journal issue | 5 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/1520-0493(2002)130<1370:APKFAS>2.0.CO;2 | |
journal fristpage | 1370 | |
journal lastpage | 1383 | |
tree | Monthly Weather Review:;2002:;volume( 130 ):;issue: 005 | |
contenttype | Fulltext |