Journal cover Journal topic
Annales Geophysicae An open-access journal of the European Geosciences Union
Ann. Geophys., 28, 1847-1857, 2010
https://doi.org/10.5194/angeo-28-1847-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
 
06 Oct 2010
Lower-thermospheric wind fluctuations measured with an FPI during pulsating aurora at Tromsø, Norway
S. Oyama1,2, K. Shiokawa1, J. Kurihara1,*, T. T. Tsuda1, S. Nozawa1, Y. Ogawa3, Y. Otsuka1, and B. J. Watkins2 1Solar-Terrestrial Environment Laboratory, Nagoya University, Nagoya, Japan
2Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA
3National Institute of Polar Research, Tokyo, Japan
*now at: Graduate School of Science, Hokkaido University, Sapporo, Japan
Abstract. Simultaneous observations were conducted with a Fabry-Perot Interferometer (FPI) at a wavelength of 557.7 nm, an all-sky camera at a wavelength of 557.7 nm, and the European Incoherent Scatter (EISCAT) UHF radar during the Dynamics and Energetics of the Lower Thermosphere in Aurora 2 (DELTA-2) campaign in January 2009. This paper concentrated on two events during periods of pulsating aurora. The lower-thermospheric wind velocity measured with the FPI showed obvious fluctuations in both vertical and horizontal components. Of particular interest is that the location of the fluctuations was found in a darker area that appeared within the pulsating aurora. During the same time period, the EISCAT radar observed sporadic enhancements in the F-region backscatter echo power, which suggests the presence of low-energy electron (1 keV or lower) precipitation coinciding with increase in amplitude of the electromagnetic wave (at the order of 10 Hz or higher). While we have not yet identified the dominant mechanism causing the fluctuations in FPI-derived wind velocity during the pulsating aurora, the frictional heating energy dissipated by the electric-field perturbations may be responsible for the increase in ionospheric thermal energy thus modifying the local wind dynamics in the lower thermosphere.

Citation: Oyama, S., Shiokawa, K., Kurihara, J., Tsuda, T. T., Nozawa, S., Ogawa, Y., Otsuka, Y., and Watkins, B. J.: Lower-thermospheric wind fluctuations measured with an FPI during pulsating aurora at Tromsø, Norway, Ann. Geophys., 28, 1847-1857, https://doi.org/10.5194/angeo-28-1847-2010, 2010.
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