Statistical Corrections to Numerical Predictions. Part IVSource: Monthly Weather Review:;1986:;volume( 114 ):;issue: 012::page 2402DOI: 10.1175/1520-0493(1986)114<2402:SCTNPP>2.0.CO;2Publisher: American Meteorological Society
Abstract: The NMC Barotropic-Mesh Model has been used to test a statistical correction procedure, designated as M-II, that was developed in Schemm et al. In the present application, statistical corrections at 12 h resulted in significant reductions of the mean-square errors of both vorticity, ?, and ?2h, where h is the 850?500 mb thickness. Predictions to 48 h demonstrated the feasibility of applying corrections at every 12 h in extended forecasts. In addition to these improvements, however, the statistical corrections resulted in a shift of error from smaller to larger-scale motions, improving the smallest scales dramatically but deteriorating the largest scales. This effect is shown to be a consequence of randomization of the residual errors by the regression equations and can be corrected by spatially high-pass filtering the field of corrections before they are applied.
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contributor author | Schemm, Jae-Kyung E. | |
contributor author | Faller, Alan J. | |
date accessioned | 2017-06-09T16:06:04Z | |
date available | 2017-06-09T16:06:04Z | |
date copyright | 1986/12/01 | |
date issued | 1986 | |
identifier issn | 0027-0644 | |
identifier other | ams-60929.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4201653 | |
description abstract | The NMC Barotropic-Mesh Model has been used to test a statistical correction procedure, designated as M-II, that was developed in Schemm et al. In the present application, statistical corrections at 12 h resulted in significant reductions of the mean-square errors of both vorticity, ?, and ?2h, where h is the 850?500 mb thickness. Predictions to 48 h demonstrated the feasibility of applying corrections at every 12 h in extended forecasts. In addition to these improvements, however, the statistical corrections resulted in a shift of error from smaller to larger-scale motions, improving the smallest scales dramatically but deteriorating the largest scales. This effect is shown to be a consequence of randomization of the residual errors by the regression equations and can be corrected by spatially high-pass filtering the field of corrections before they are applied. | |
publisher | American Meteorological Society | |
title | Statistical Corrections to Numerical Predictions. Part IV | |
type | Journal Paper | |
journal volume | 114 | |
journal issue | 12 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/1520-0493(1986)114<2402:SCTNPP>2.0.CO;2 | |
journal fristpage | 2402 | |
journal lastpage | 2417 | |
tree | Monthly Weather Review:;1986:;volume( 114 ):;issue: 012 | |
contenttype | Fulltext |