Geomagnetic conjugate observations of equatorial airglow depletions

[1] We report for the first time large-scale equatorial F-region airglow depletions extending to low-midlatitudes in both hemispheres. The observational sites were located at low-midlatitude geomagnetic conjugate points. Clear depletions of 630.0-nm airglow intensity due to equatorial plasma bubbles were simultaneously observed with two all-sky imagers at Sata, Japan (magnetic latitude 24°N), and its geomagnetic conjugate point, Darwin, Australia (magnetic latitude 22°S), on the night of November 12, 2001. Airglow depletion regions with east-west scale sizes of 40–100 km extend poleward. The maximum apex altitude of the plasma bubbles is about 1,700 km over the geomagnetic equator. The depletions move eastward at about 100 m/s, without changing their structures. The Darwin depletion structures mapped onto the northern hemisphere along the geomagnetic field coincide closely with structures in the Sata images, even for the 40-km structure. These observations indicate that plasma depletions in the equatorial ionosphere elongate along the geomagnetic field lines.

[1]  Michael C. Kelley,et al.  The Earth's Ionosphere : Plasma Physics and Electrodynamics , 1989 .

[2]  E. J. Weber,et al.  Coordinated airborne and satellite measurements of equatorial plasma depletions , 1982 .

[3]  M. Satoh,et al.  Development of Optical Mesosphere Thermosphere Imagers (OMTI) , 1999 .

[4]  Bodo W. Reinisch,et al.  Investigations of thermospheric‐ionospheric dynamics with 6300‐Å images from the Arecibo Observatory , 1997 .

[5]  J. Meriwether,et al.  Testing the thermospheric neutral wind suppression mechanism for day-to-day variability of equatorial spread F , 2001 .

[6]  C. E. Barton,et al.  International Geomagnetic Reference Field : The seventh generation , 1997 .

[7]  Takashi Maruyama,et al.  Longitudinal variability of annual changes in activity of equatorial spread F and plasma bubbles , 1984 .

[8]  Michael C. Kelley,et al.  The earth's ionosphere , 1989 .

[9]  K. Shiokawa,et al.  Integrating-sphere calibration of all-sky cameras for nightglow measurements , 2000 .

[10]  M. Kelley,et al.  Nonlinear evolution of equatorial spread F: 2. Gravity wave seeding of Rayleigh‐Taylor instability , 1996 .

[11]  T. Maruyama A diagnostic model for equatorial spread F, 1, Model description and application to electric field and neutral wind effects , 1988 .

[12]  P. Fagundes,et al.  Observations of equatorial F region plasma bubbles using simultaneous OI 777.4 nm and OI 630.0 nm imaging , 2001 .

[13]  P. Fagundes,et al.  Transequatorial F-region ionospheric plasma bubbles: solar cycle effects , 2000 .

[14]  H. Rishbeth Thermospheric winds and the F-region: A review , 1972 .

[15]  S. Basu,et al.  The multi‐instrumented studies of equatorial thermosphere aeronomy scintillation system: Climatology of zonal drifts , 1996 .

[16]  S. Basu,et al.  Magnetic‐flux‐tube‐integrated evolution of equatorial ionospheric plasma bubbles , 1998 .

[17]  L. H. Brace,et al.  Conjugate occurrence of the electric field fluctuations in the nighttime midlatitude ionosphere , 1995 .

[18]  E. R. Paula,et al.  Effects of the vertical plasma drift velocity on the generation and evolution of equatorial spread F , 1999 .

[19]  E. Bonelli,et al.  The prereversal enhancement of the zonal electric field in the equatorial ionosphere , 1986 .