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Lower thermospheric composition changes derived from optical and radar data taken at Sondre Stromfjord during the great magnetic storm of February 1986

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/90JA02460· OSTI ID:5186634
; ; ;  [1];  [2]
  1. Aerospace Corp., Los Angeles, CA (USA)
  2. Computational Physics, Inc., Annadale, VA (USA)
Several nights of optical and radar data were obtained from February 3 to 10, 1986 at Sondre Stromfjord, Greenland during a great geomagnetic storm when Ap reached 202. These data, excluding O I (630.0 nm), were used to monitor changes in O and O{sub 2} densities in the region from 100 to 200 km and are consistent with results of Hecht et al. (1989) wherein the O I (630.0 nm) emission was used. That is, there were large depletions of O in the E region during the peak of the storm. Using 24-hour Ap values both MSIS-83 and MSIS-86 underestimated the depletion of O during the storm. MSIS-86 did noticeably worse than did MSIS-83, probably a result of the low exospheric temperature predicted by MSIS-86. However, when 3-hour ap values were used both models did better in predicting the measured O depletions, although MSIS-86 again was less successful than was MSIS-83. The data results also show that the enchancements in O{sub 2} were less than predicted by MSIS models in either mode. From 0200-0230 UT on February 9, 1986, a time just after the peak of geomagnetic activity as measured by Kp, the O mixing ratio near 135 km was found to increase by nearly a factor of 2. This increase is consistent with the passage of an atmospheric gravity wave through this altitude region providing that the scale height of O above 140 km is greater than predicted by the model.
OSTI ID:
5186634
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 96:A4; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English

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