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Diagnosis and modelling of Tropical Cyclone Catarina (2004) Ron McTaggart-Cowan and Lance Bosart University at Albany, State University of New York
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Outline ● Case introduction and background ● Diagnostic investigation of Catarina's origins – Extended analysis for March 2004 – Climatology of persistent Rex blocking in the South Atlantic ● Modelling Catarina's spin-up as a tropical system ● Discussion and future directions
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Introduction and Background ● Extratropical disturbance first identified 18/19 ● Tropical structures begin to appear 00/24 ● System becomes tropical just after 00/25 ● Winds of 75-85 kts develop by 06/28 Storm track and intensity estimates based on best track by Roger Edson
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Introduction and Background 0000 UTC 12 March 2004
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Introduction and Background 0000 UTC 13 March 2004
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Introduction and Background 0000 UTC 14 March 2004
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Introduction and Background 0000 UTC 15 March 2004
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Introduction and Background 0000 UTC 16 March 2004
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Introduction and Background 0000 UTC 17 March 2004
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Introduction and Background 0000 UTC 18 March 2004
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Introduction and Background 0000 UTC 19 March 2004
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Introduction and Background 0000 UTC 20 March 2004
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Introduction and Background 0000 UTC 12 March 2004
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Introduction and Background 0000 UTC 22 March 2004
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Introduction and Background 0000 UTC 23 March 2004
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Introduction and Background 0000 UTC 24 March 2004
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Introduction and Background 0000 UTC 25 March 2004
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Introduction and Background 0000 UTC 26 March 2004
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Introduction and Background 0000 UTC 27 March 2004
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Introduction and Background 0000 UTC 28 March 2004
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Introduction and Background 0000 UTC 29 March 2004
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Introduction and Background 0000 UTC 20 March 2004
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Introduction and Background 0000 UTC 21 March 2004
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Introduction and Background 0000 UTC 22 March 2004
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Introduction and Background 0000 UTC 23 March 2004
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Introduction and Background 0000 UTC 24 March 2004
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Introduction and Background 0000 UTC 25 March 2004
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Introduction and Background 0000 UTC 26 March 2004
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Introduction and Background 0000 UTC 27 March 2004
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Introduction and Background 0000 UTC 28 March 2004
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Introduction and Background 0000 UTC 29 March 2004
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Introduction and Background 0915 UTC 25 2028 UTC 25 0849 UTC 26 2116 UTC 270832 UTC 272002 UTC 26 >45 kts QuikScat and GOES imagery from FNMOC
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Introduction and Background NOAA NESDIS Mean SST for 24-27 March 2004 NOAA NESDIS Operational SST anomaly for 26 March 2004 24 28 -202 26
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Diagnostic Study ● Investigate the origins of the tropical disturbance in terms of the large-scale flow near South America in late March 2004 ● Determine what - if any - distinct features led to the rare tropical transition/cyclogenesis – Persistent troughing east of Brazil – Maintenance of a Rex block in the are over a period of two weeks
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Diagnostic Study 0000 UTC 12 March 2004
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Diagnostic Study 0000 UTC 13 March 2004
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Diagnostic Study 0000 UTC 14 March 2004
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Diagnostic Study 0000 UTC 15 March 2004
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Diagnostic Study 0000 UTC 16 March 2004
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Diagnostic Study 0000 UTC 17 March 2004
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Diagnostic Study 0000 UTC 18 March 2004
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Diagnostic Study 0000 UTC 19 March 2004
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Diagnostic Study 0000 UTC 20 March 2004
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Diagnostic Study 0000 UTC 21 March 2004
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Diagnostic Study 0000 UTC 22 March 2004
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Diagnostic Study 0000 UTC 23 March 2004
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Diagnostic Study 0000 UTC 24 March 2004
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Diagnostic Study 0000 UTC 25 March 2004
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Diagnostic Study 0000 UTC 26 March 2004
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Diagnostic Study 0000 UTC 27 March 2004
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Diagnostic Study 0000 UTC 28 March 2004
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Diagnostic Study 0000 UTC 29 March 2004 3
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Diagnostic Study 0000 UTC 20 March 2004 1 2 A B
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Diagnostic Study 0000 UTC 21 March 2004 2 1 A B
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Diagnostic Study 0000 UTC 22 March 2004 2 1 B
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Diagnostic Study 0000 UTC 23 March 2004 3 2 1 B
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Diagnostic Study 0000 UTC 24 March 2004 3 2 1 C
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Diagnostic Study 0000 UTC 25 March 2004 3 2 1 C
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Diagnostic Study 0000 UTC 26 March 2004 3 2
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Diagnostic Study 0000 UTC 27 March 2004 3 2
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Diagnostic Study 0000 UTC 28 March 2004 3
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Diagnostic Study 0000 UTC 29 March 2004 3
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Diagnostic Study 0000 UTC 23 March 2004
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Diagnostic Study 0000 UTC 25 March 2004
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Diagnostic Study 0000 UTC 27 March 2004
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Diagnostic Study ● Repeated trough reinforcements off the Brazilian east coast from 12-28 March 2004 ● Repeated poleward advection of low-PV air from the Pacific over same period ● The resulting Rex block helps to reduce the deep-layer shear over the developing system ● But how often does this happen?
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Diagnostic Study Mean 500 hPa Height Anomaly 16-29 March 2004
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Diagnostic Study NCEP/NCAR Reanalysis Mean 300 hPa heights for 16- 29 March 2004 Average anomalous 300 hPa heights for 16-29 March 2004
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Diagnostic Study 0000 UTC 18 March 2004
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Diagnostic Study 0000 UTC 20 March 2004
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Diagnostic Study 0000 UTC 22 March 2004
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Diagnostic Study 0000 UTC 24 March 2004
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Diagnostic Study 0000 UTC 26 March 2004
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Diagnostic Study 0000 UTC 28 March 2004
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Diagnostic Study Feb-March
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● The in-situ development of the system suggests a combination of physical and dynamical forcings ● Cool SSTs (~26C) were at or below climatology ● Lack of in-situ observations make analysis of the case problematic ● A good simulation of the development will provide a consistent dataset from which to continue higher-resolution diagnostics Modelling Study
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● Track of the system is well modelled 12/25 – 00/28 ● Storm remains weak throughout the simulation Modelling Study Simulated Track Best Track (Roger Edson)
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Modelling Study 00 h forecast 1200 UTC 25 March A B
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Modelling Study 00 h forecast 1200 UTC 25 March
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Modelling Study A B 00 h forecast 1200 UTC 25 March
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Modelling Study A B 00 h forecast 1200 UTC 25 March
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Modelling Study 00 h forecast 1200 UTC 25 March
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Modelling Study 48 h forecast 1200 UTC 27 March
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Modelling Study 60 h forecast 0000 UTC 28 March
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Modelling Study A B 72 h forecast 1200 UTC 28 March
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Modelling Study 72 h forecast 1200 UTC 28 March
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Modelling Study A B 72 h forecast 1200 UTC 28 March
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Modelling Study A B 72 h forecast 1200 UTC 28 March
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Modelling Study 72 h forecast 1200 UTC 28 March
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● The development of TC Catarina occurred under an unusually persistent Rex block off the Brazilian east coast ● Repeated injections of high (low) PV air to the ridge (trough) maintained the block and reduced the shear above the developing system ● Large-scale dynamics and steering are well represented in simulations, but inadequate initial moisture reduces spin-up Summary and Discussion
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● Reanalyze case using higher-resolution experimental Brazilian analyses ● Investigate the source of the vapour deficit in the operational analyses ● Perform moisture-based sensitivity studies in an effort to better simulate the observed development Future Directions
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