Validation of Cloud-Resolving Model Background Data for Cloud Data AssimilationSource: Monthly Weather Review:;2009:;volume( 138 ):;issue: 003::page 781DOI: 10.1175/2009MWR3012.1Publisher: American Meteorological Society
Abstract: Results from a cloud-resolving model are systematically compared with a variety of observations, both ground based and satellite, in order to better understand the mean background errors and their correlations. This is a step in the direction of developing a background error covariance matrix for use in cloud data assimilation. Observation sources include the Geostationary Operational Environmental Satellite (GOES), the Atmospheric Emitted Radiance Interferometer (AERI), a microwave radiometer (MWR), radiosonde, and cloud radar. When exploring model biases in temperature, precipitable water vapor, and liquid water path, a warm and moist bias at night and a cool and dry bias during the day are observed. Values for the background decorrelation length of water variables are determined. In addition, a dynamic cloud mask is presented to give more control in the assimilation of cloudy satellite radiances, allowing different cloud types to be excluded from the assimilation as well as establishing values for the maximum residuals to be considered.
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contributor author | Polkinghorne, Rosanne | |
contributor author | Vukicevic, Tomislava | |
contributor author | Evans, K. Franklin | |
date accessioned | 2017-06-09T16:32:18Z | |
date available | 2017-06-09T16:32:18Z | |
date copyright | 2010/03/01 | |
date issued | 2009 | |
identifier issn | 0027-0644 | |
identifier other | ams-69613.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4211302 | |
description abstract | Results from a cloud-resolving model are systematically compared with a variety of observations, both ground based and satellite, in order to better understand the mean background errors and their correlations. This is a step in the direction of developing a background error covariance matrix for use in cloud data assimilation. Observation sources include the Geostationary Operational Environmental Satellite (GOES), the Atmospheric Emitted Radiance Interferometer (AERI), a microwave radiometer (MWR), radiosonde, and cloud radar. When exploring model biases in temperature, precipitable water vapor, and liquid water path, a warm and moist bias at night and a cool and dry bias during the day are observed. Values for the background decorrelation length of water variables are determined. In addition, a dynamic cloud mask is presented to give more control in the assimilation of cloudy satellite radiances, allowing different cloud types to be excluded from the assimilation as well as establishing values for the maximum residuals to be considered. | |
publisher | American Meteorological Society | |
title | Validation of Cloud-Resolving Model Background Data for Cloud Data Assimilation | |
type | Journal Paper | |
journal volume | 138 | |
journal issue | 3 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/2009MWR3012.1 | |
journal fristpage | 781 | |
journal lastpage | 795 | |
tree | Monthly Weather Review:;2009:;volume( 138 ):;issue: 003 | |
contenttype | Fulltext |