A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
Statistical Evaluation of the Wet Season Atmospheric Mesoscale Campaign – LBAand GTS Observations used in RPSAS with CPTEC Eta modelRosângela Cintra, José A. Aravéquia, Julio Tóta,Dirceu Herdies, Jose P. BonattiCentro de Previsão de Tempo e Estudos Climáticos - CPTEC/INPERodovia Presidente Dutra, km 4012630-000 -Cachoeira Paulista - SPe-mail:rcintra@cptec.inpe.brAbstractTo improve the skill of the CPTEC regional model was developed and implemented aanalysis system, called Regional Physical-space Statistical Analysis System (RPSAS),that make use of the core system PSAS from Data Assimilation Office (DAO) on theGSFC/NASA. The RPSAS has ben designed as an improvement over the currentOptimal Interpolation (OI) based on the Data Assimilation System (DAS). FromJanuary to February 1999, during AMC-WET/LBA campaign, comparisons of theObservation Data Stream (ODS) and the RPSAS analysis fields were made using theEta six hour forecast fields (first guess). The Eta model was integrated daily for 00, 06,12 and 18 GMT using initial conditions from RPSAS analyses. The statistical indexeswere calculated with the purpose of evaluating the quality of the analysis. Theobservations minus analysis and the observations minus first guess for geopotentialheight and humidity at the levels 850, 500 and 300 hPa levels were used to generatemean bias score and standard deviation (RMS) for each region to produce a statisticalevaluaton of the observing system for South America. The first results show mean biasscore for geopotential height amplitude on 500 hPa of approximately 16 mgp at 00Z , 28mgp at 06Z, 8 mgp at 12Z, and 14 mgp at 18Z.
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St<strong>at</strong>istical Evalu<strong>at</strong>ion of <strong>the</strong> Wet Season Atmospheric Mesoscale Campaign – LBAand GTS Observ<strong>at</strong>ions used in RPSAS <strong>with</strong> CPTEC Eta modelRosângela Cintra, José A. Aravéquia, Julio Tóta,Dirceu Herdies, Jose P. Bon<strong>at</strong>tiCentro de Previsão de Tempo e Estudos Climáticos - CPTEC/INPERodovia Presidente Dutra, km 4012630-000 -Cachoeira Paulista - SPe-mail:rcintra@cptec.inpe.brAbstractTo improve <strong>the</strong> skill of <strong>the</strong> CPTEC regional model was developed and implemented aanalysis system, called Regional Physical-space St<strong>at</strong>istical Analysis System (RPSAS),th<strong>at</strong> make use of <strong>the</strong> core system PSAS from D<strong>at</strong>a Assimil<strong>at</strong>ion Office (DAO) on <strong>the</strong>GSFC/NASA. The RPSAS has ben designed as an improvement over <strong>the</strong> currentOptimal Interpol<strong>at</strong>ion (OI) based on <strong>the</strong> D<strong>at</strong>a Assimil<strong>at</strong>ion System (DAS). FromJanuary to February 1999, during AMC-WET/LBA campaign, comparisons of <strong>the</strong>Observ<strong>at</strong>ion D<strong>at</strong>a Stream (ODS) and <strong>the</strong> RPSAS analysis fields were made using <strong>the</strong>Eta six hour forecast fields (first guess). The Eta model was integr<strong>at</strong>ed daily for 00, 06,12 and 18 GMT using initial conditions from RPSAS analyses. The st<strong>at</strong>istical indexeswere calcul<strong>at</strong>ed <strong>with</strong> <strong>the</strong> purpose of evalu<strong>at</strong>ing <strong>the</strong> quality of <strong>the</strong> analysis. Theobserv<strong>at</strong>ions minus analysis and <strong>the</strong> observ<strong>at</strong>ions minus first guess for geopotentialheight and humidity <strong>at</strong> <strong>the</strong> levels 850, 500 and 300 hPa levels were used to gener<strong>at</strong>emean bias score and standard devi<strong>at</strong>ion (RMS) for each region to produce a st<strong>at</strong>isticalevalu<strong>at</strong>on of <strong>the</strong> observing system for South America. The first results show mean biasscore for geopotential height amplitude on 500 hPa of approxim<strong>at</strong>ely 16 mgp <strong>at</strong> 00Z , 28mgp <strong>at</strong> 06Z, 8 mgp <strong>at</strong> 12Z, and 14 mgp <strong>at</strong> 18Z.