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contributor authorHertzog, Albert
contributor authorCocquerez, Philippe
contributor authorGuilbon, René
contributor authorValdivia, Jean-Noël
contributor authorVenel, Stéphanie
contributor authorBasdevant, Claude
contributor authorBoccara, Gillian
contributor authorBordereau, Jérôme
contributor authorBrioit, Bernard
contributor authorVial, François
contributor authorCardonne, Alain
contributor authorRavissot, Alain
contributor authorSchmitt, Éric
date accessioned2017-06-09T16:20:36Z
date available2017-06-09T16:20:36Z
date copyright2007/12/01
date issued2007
identifier issn0739-0572
identifier otherams-66124.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207426
description abstractIn September and October 2005, the Stratéole/Vorcore campaign flew 27 superpressure balloons from McMurdo, Antarctica, into the stratospheric polar vortex. Long-duration flights were successfully achieved, 16 of those flights lasting for more than 2 months. Most flights were terminated because they flew out of the authorized flight domain or because of energy shortage in the gondola. The atmospheric pressure (1-Pa precision) was measured every minute during the flights, whereas air temperature observations (0.25-K accuracy) and balloon positions (absolute GPS observations, 10-m accuracy) were obtained every 15 min. Fifteen-minute-averaged horizontal velocities of the wind were deduced from the successive balloon positions with a corresponding accuracy ?0.1 m s?1. The collected dataset (more than 150 000 independent observations) provides a thorough high-resolution sampling of the polar lower stratosphere in the Southern Hemisphere from its wintertime state up to the establishment of the summer circulation in December?January. Most of the balloons stayed inside the vortex until its final breakdown, although a few were ejected toward the midlatitudes in November during filamention events associated with an increase in planetary wave activity. The balloons behaved as quasi-Lagrangian tracers during the first part of the campaign (quiescent vortex) and after the vortex breakdown in early December. Large-amplitude mountain gravity waves were detected over the Antarctic Peninsula and caused one flight termination associated with the sudden burst in the balloon superpressure.
publisherAmerican Meteorological Society
titleStratéole/Vorcore—Long-duration, Superpressure Balloons to Study the Antarctic Lower Stratosphere during the 2005 Winter
typeJournal Paper
journal volume24
journal issue12
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/2007JTECHA948.1
journal fristpage2048
journal lastpage2061
treeJournal of Atmospheric and Oceanic Technology:;2007:;volume( 024 ):;issue: 012
contenttypeFulltext


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