Three-Dimensional Covariance Functions for NOGAPS DataSource: Monthly Weather Review:;1999:;volume( 127 ):;issue: 010::page 2293Author:Franke, Richard
DOI: 10.1175/1520-0493(1999)127<2293:TDCFFN>2.0.CO;2Publisher: American Meteorological Society
Abstract: Height innovation data for a 2-month period from NOGAPS was analyzed to obtain height prediction and observation error covariances. Different methods of weighting the data in least squares approximations of the spatial covariance data were investigated using the second-order autoregressive (SOAR) correlation function, both with and without an additive constant (varying with pressure level). Based on the properties of the derived covariance matrices and the SOAR parameters, the SOAR without an additive constant was used for the horizontal approximations. The vertical correlations were fit using a combination of SOAR plus an additive constant and a transformation of the logP coordinate to another coordinate to achieve a best fit. The resulting three-dimensional approximation is partially separable, being the product of the horizontal covariance function (which depends on height) and the vertical correlation function. Figures demonstrating various aspects of the process and the results are given.
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| contributor author | Franke, Richard | |
| date accessioned | 2017-06-09T16:12:38Z | |
| date available | 2017-06-09T16:12:38Z | |
| date copyright | 1999/10/01 | |
| date issued | 1999 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-63383.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4204380 | |
| description abstract | Height innovation data for a 2-month period from NOGAPS was analyzed to obtain height prediction and observation error covariances. Different methods of weighting the data in least squares approximations of the spatial covariance data were investigated using the second-order autoregressive (SOAR) correlation function, both with and without an additive constant (varying with pressure level). Based on the properties of the derived covariance matrices and the SOAR parameters, the SOAR without an additive constant was used for the horizontal approximations. The vertical correlations were fit using a combination of SOAR plus an additive constant and a transformation of the logP coordinate to another coordinate to achieve a best fit. The resulting three-dimensional approximation is partially separable, being the product of the horizontal covariance function (which depends on height) and the vertical correlation function. Figures demonstrating various aspects of the process and the results are given. | |
| publisher | American Meteorological Society | |
| title | Three-Dimensional Covariance Functions for NOGAPS Data | |
| type | Journal Paper | |
| journal volume | 127 | |
| journal issue | 10 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1999)127<2293:TDCFFN>2.0.CO;2 | |
| journal fristpage | 2293 | |
| journal lastpage | 2308 | |
| tree | Monthly Weather Review:;1999:;volume( 127 ):;issue: 010 | |
| contenttype | Fulltext |