Strateole/Vorcore - Long-duration, superpressure balloons to study the antarctic lower stratosphere during the 2005 winter

被引:46
|
作者
Hertzog, Albert [1 ]
Cocquerez, Philippe [2 ]
Basdevant, Claude [3 ]
Boccara, Gillian [3 ]
Bordereau, Jerome [3 ]
Brioit, Bernard [3 ]
Cardonne, Alain [4 ]
Guilbon, Rene [2 ]
Ravissot, Alain [4 ]
Schmitt, Eric [4 ]
Valdivia, Jean-Noel [2 ]
Venel, Stephanie [2 ]
Vial, Francois [3 ]
机构
[1] Univ Paris 06, Meteorol Dynam Lab, IPSL, CNRS, Palaiseau, France
[2] Ctr Natl Etud Spatiales, F-31055 Toulouse, France
[3] Ecole Polytech, Meteorol Dynam Lab, IPSL, CNRS, Palaiseau, France
[4] Ctr Natl Etud Spatiales, Aire sur Ladour, France
关键词
D O I
10.1175/2007JTECHA948.1
中图分类号
P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
In September and October 2005, the Strateole/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 less than or similar to 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.
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收藏
页码:2048 / 2061
页数:14
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