Modelling study of Mesoscale Cyclogenesis over Ross Sea,Antarctica,on February 18,1988

• Main Authors: M. Stortini, S. Marchesi, MORELLI, Sandra
• Other Authors: M., Stortini, Morelli, Sandra, S., Marchesi
• Format: Article in Journal/Newspaper
• Language: English
• Published: Societa Italiana di Fisica:Via Saragozza 12 Subs Service, I 40123 Bologna Italy:011 39 051 331554, EMAIL: [e-mail], INTERNET: http://www.sif.it, Fax: [phone] 2000
• Subjects: Mesoscale cyclogenesi; numerical simulation; katabatic wind; Ross Sea; Victoria Land; Terra Nova Bay; Eta; Antarc*; Antarctica
• Online Access: http://hdl.handle.net/11380/455538

This paper examines the development of a summer event of mesoscale cyclogenesis off the coast of Victoria Land in the presence of katabatic winds, by means of numerical simulations. These refer to the period from 00 UTC 17 February to 00 UTC 19 February 1988 and were performed using the hydrostatic ETA (1993 version) limited area model with resolution 55 km x 55 km x 17 levels. The ETA model reproduces katabatic winds from Terra Nova Bay and a trough on the southwestern Ross Sea. A cyclonic vortex is simulated in the trough, even though it is weaker than the one present in the analyses initialized by the European Center for Medium Range Weather Forecast (Reading, UK). Idealized simulations with varied surface conditions were also performed. In particular, an ice-covered ocean acts to weaken the atmospheric phenomena, while a no-mountain simulation emphasizes the influence of the orography and the cold winds from the coast of Victoria Land on the mesocyclonic activity.