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contributor authorSinclair, Mark R.
date accessioned2017-06-09T16:10:23Z
date available2017-06-09T16:10:23Z
date copyright1995/06/01
date issued1995
identifier issn0027-0644
identifier otherams-62564.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203470
description abstractThis study surveys life cycle characteristics of cyclones in the Southern Hemisphere (SH). An objective technique for locating instances of cyclone formation, intensification, maturation, and decay is applied to a 7-year dataset of SH cyclone positions, obtained from an automated finding and tracking scheme based on twice-daily ECMWF analyses during 1980?86. Geostrophic vorticity ?g at 1000 hPa is used to locate cyclones and determine their intensity. Cyclones form and develop within middle latitudes and migrate eastward and poleward during their lives. Preferred genesis and cyclogenesis regions include eastern coasts of Australia and South America in winter, and leeward of the Andes and near the baroclinic zones associated with the principal upper-tropospheric jet streams year round. Over open water, winter cyclones tend to form and intensify near zones of strongest SST gradient. Rapid cyclogenesis is most frequent east of South America, southeast of Africa, south of Australia, and near New Zealand. Large differences were found between the geographical distribution of developing cyclones as inferred from ?g, tendencies and those obtained from central pressure change. The latter were found to be highly dependent on cyclone motion relative to the background pressure field.
publisherAmerican Meteorological Society
titleA Climatology of Cyclogenesis for the Southern Hemisphere
typeJournal Paper
journal volume123
journal issue6
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1995)123<1601:ACOCFT>2.0.CO;2
journal fristpage1601
journal lastpage1619
treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 006
contenttypeFulltext


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