1.6
On the Strategies for the 4D-Var Assimilation of TOMS Ozone Observation into Atmospheric Models
PAPER WITHDRAWN
M. Pondeca, Florida State University, Tallahassee, Florida; and X. Zou
Results from a case study of the four-dimensional variational (4D-Var) assimilation of vertically integrated TOMS ozone observations and rawinsonde data into the Penn State / NCAR MM5 model will be presented. The synoptic situation involves an intense winter storm that produced heavy snow- and rainfall over Maryland on the 25th of January 2001. Operational models failed to accurately predict both the intensity and path of the low pressure system responsible for the storm. In particular, model projections were for most of the storm activity to occur offshore, over the Atlantic Ocean. Using the NCEP analysis to form the model initial condition, our a posteriori control forecast with the MM5 model also failed to account for the intensity and position of the cyclone. The Cressman objective analysis of rawinsonde wind, temperature and humidity data which is commonly used in the ``MM5 package'' to improve the first-guess NCEP analysis was found to have very little impact on the cyclone forecast.
The alternate 4D-Var assimilation of the same rawinsonde observations was found to produce measurable improvements in the cyclone intensity and position. It is hoped that further improvements can be attained through the 4D-Var assimilation of vertically integrated TOMS ozone observations. However, work carried out thus far suggests that TOMS ozone observations are likely to have an impact on the forecast only if combined with additional information that constrains the model fields in the medium and lower-troposphere. This is because most of the tropospheric ozone is located above the tropopause. The much needed information on the model tropospheric fields can be obtained through the inclusion of more types of observations in the assimilation experiments (e.g. satellite derived rainfall rates). It also anticipated that, through the vertical correlations, the background error covariance matrix will be instrumental in correctly constraining the analysis increments in the troposphere that result from the assimilation of TOMS ozone observations. A method of evaluating the background error covariance matrix on the basis of an ensemble of background error fields that are assumed to provide a good sample of the distribution of all possible error structures will be presented. Using the exact definition of the background error covariance matrix, the auto-correlations and multivariate cross-correlations are obtained through ensembles of vector products. Computational feasibility is achieved by restricting the number of error fields to ten and assuming that the subspace spanned by the five leading eigenvectors of the (ensemble) background error covariance matrix contains all the information on the statistics of the background errors. The performance of the 4D-Var assimilation system that uses such a background error covariance matrix will be compared with the previous system that only uses a diagonal matrix of error variances. A discussion of our ongoing research with an emphasis on the best strategies for assimilating TOMS ozone into atmospheric models will be offered.
Session 1, Effective Assimilation of the Vast Observational Datasets Becoming Available
Monday, 14 January 2002, 9:30 AM-2:44 PM
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