Ionospheric response to 2009 sudden stratospheric warming in the Northern Hemisphere. Issue 12 (5th December 2014)

• Record Type: Journal Article
• Authors: Oyama, K.‐I.; Jhou, J. T.; Lin, J. T.; Lin, C.; Liu, H.; Yumoto, K.
• Is Part Of: Journal of geophysical research. Volume 119:Issue 12(2014:Dec.)
• Page Start: 10, 260
• Page End: 10, 275
• Publication Date: 2014-12-05
• Subjects: sudden stratosphere warming -- F region ionosphere -- electrodynamics -- equator; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1002/2014JA020014
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: We study the behavior of the F region ionosphere in the Northern Hemisphere during the sudden stratospheric warming period of 19–30 January 2009 by using FORMOSAT‐3/Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) ionosphere data ( Nm F 2, hm F 2, and height profile). We concentrated our study in the longitude bands 30°E–30°W, as well as 150°E–150°W, where no detailed study has been reported so far. At low magnetic latitude, the Nm F 2 decreases except during 09–12 LT: in the latitude zone of 20–40° Nm F 2 shows an increase of 30% during 09–12 LT. At higher magnetic latitude the Nm F 2 shows an increase during daytime and a reduction in the evening (21–03 LT). There is a latitude zone where Nm F 2 does not change. The latitude seems to correspond to the latitude where atmospheric temperature does not change. The behavior of the Nm F 2 seems to suggest a reduction of neutral density in low latitude and increase of neutral density in higher latitude. During the period of day of year (DOY) 25–31, the Nm F 2 shows a drastic reduction only during 06–09 LT in low latitudes, which is slightly away from geomagnetic equator. This special feature which occurred during declining phase of the sudden stratospheric warming (SSW) might be explained as due to enhanced dynamo electric field. The study suggests global change of the thermosphere including dynamo region, in spite of the fact that SSW is a high‐latitude phenomenon which occurred much below the height region of thermosphere. Key Points: A latitude region exists where Nm F2 does not change during SSW Extremely reduced Nm F2 appears in low geomagnetic altitude at 06–09 LT Similar ionospheric feature appears at two longitude zones