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Ann. Geophys., 24, 1257-1266, 2006
www.ann-geophys.net/24/1257/2006/
© European Geosciences Union 2006


Sporadic sodium and E layers observed during the summer 2002 MaCWAVE/MIDAS rocket campaign

B. P. Williams1, C. L. Croskey2, C. Y. She3, J. D. Mitchell2, and R. A. Goldberg4
1Northwest Research Associates, Colorado Research Associates division, Boulder, CO, USA
2Communications and Space Sciences Laboratory, Electrical Engineering Department, Pennsylvania State University, University Park, Pennsylvania, USA
3Department of Physics, Colorado State University, Fort Collins, Colorado, USA
4NASA/Goddard Space Flight Center, Laboratory for Solar and Space Physics, Greenbelt, MD, USA

Abstract. On 5 July 2002, a MaCWAVE (Mountain and Convective Waves Ascending VErtically) payload launched from Andøya Rocket Range, Norway, observed narrow enhanced layers of electron density that were nearly coincident with sporadic sodium layers measured by the Weber sodium lidar at the nearby ALOMAR Observatory. We investigate the formation mechanism of these layers using the neutral wind and temperature profiles measured directly by the lidar and the vertical motion deduced from the sodium mixing ratio. Through comparisons of the lidar data to the sporadic E in situ data, we find support for the concentration and downward motion of ions to an altitude where chemical models predict the rapid conversion of sodium ions to neutral sodium.

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