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Balloon observations of temporal and spatial fluctuations in stratospheric conductivity
Institution:1. Physics Department, University of Houston, 617 Science and Research I, Houston, TX 77204-5005, USA;2. Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310, USA;3. National Institute of Polar Research, Kaga 1-chome, Itabashi-ku, Tokyo 173-8515, Japan;4. The Institute of Space and Astronautical Science, Sagamihara, Kanagawa 229-8510, Japan;5. Institute of Physics, Kanagawa University, Kanagawa-ku, Yokohama 221-8686, Japan;6. Faculty of Engineering, Tokai University, Hiratsuka, Kanagawa 259-1292, Japan;7. Faculty of Science, Osaka City University, Sumiyoshi-ku, Osaka 558-8585, Japan;8. Faculty of Engineering, Toyama Prefectural University, Toyama 939-0398, Japan;1. Center for Environmental Survey, Vidyanagar Society 29/251, Ahmedabad, Gujarat 380015, India;2. Physical Research Laboratory, Navrangpura, Ahmedabad, Gujarat 380009, India
Abstract:The first campaign of the Polar Patrol Balloon (PPB) experiment (1st-PPB) was carried out at Syowa Station in Antarctica during 1990–1991 and 1992–1993. Based on the results of the 1st-PPB experiment, the next campaign (2nd-PPB) was carried out in the austral summer of 2002–2003. This paper will present stratospheric conductivity results from the 2nd-PPB experiment. In that experiment, three balloons were launched for the purpose of upper atmosphere physics observation (three balloons). Payloads of these three flights were identical with each other, and were launched as close together in time as allowed by weather conditions to constitute a cluster of balloons during their flights. Such a “Balloon Cluster” is suitable to observe temporal evolution and spatial distribution of phenomena in the ionospheric regions and boundaries that the balloons traversed during their circumpolar trajectory. More than 20 days of simultaneous fair weather 3-axis electric field and stratospheric conductivity data were obtained at geomagnetic latitudes ranging from sub-auroral to the polar cap. Balloon separation varied from ~60 to >1000 km. This paper will present stratospheric conductivity observations with emphasis on the temporal and spatial variations that were observed.
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