Identification of Night-Time F- Region Currents from CHAMP Satellite Observations over Equatorial Africa

CHAMP Satellite Observations

DOI:

https://doi.org/10.14331/ijfps.2013.330045

Keywords:

Ionosphere, Equatorial ionosphere, ionospheric current systems, magnetic field

Abstract

The F-region currents are generally weak and difficult to detect. However, their contributions to the earth’s magnetic field variations are significant and cannot be ignored by the field modelers. CHAMP satellite has therefore provided a perfect opportunity to investigate the in-situ F-region currents on the night side of the equatorial region. The magnitudes of the current along all the three components of the earth’s magnetic field (X, Y, Z) are investigated. However, in this paper, we present only the results on the Y-component where interesting magnetic residuals were observed. The X and Z-components were rather masked in much noise and would require further filtering. The currents appear in both the pre-midnight and post-midnight sectors and are spatially confined to the equatorial region bounded by the Appleton anomaly. The magnetic residuals are generally observed in the northern hemisphere of an order of 0.8nT, which gives a height-integrated current density of about 1.3mA/m.

Downloads

Download data is not yet available.

References

Campbell, W. H. (2003). Introduction to geomagnetic fields: Cambridge University Press.

Kelley, M. (1989). The Earth’s Ionosphere: Plasma Physics and Electrodynamics, Int. Geophys. Ser, 43, 437-455.

Kelley, M. C. (2009). The Earth's ionosphere: plasma physics and electrodynamics (Vol. 96): Academic Press.

Lühr, H., Maus, S., & Rother, M. (2004). Noon-time equatorial electrojet: Its spatial features as determined by the CHAMP satellite. Journal of geophysical research, 109(A1), A01306.

Lühr, H., Maus, S., Rother, M., & Cooke, D. (2002). First in-situ observation of night-time F region currents with the CHAMP satellite. Geophysical research letters, 29(10), 1489.

Maus, S., & Lühr, H. (2006). A gravity-driven electric current in the Earth's ionosphere identified in CHAMP satellite magnetic measurements. Geophysical research letters, 33(2), L02812.

Maus, S., & MacMillan, S. (2005). 10th generation international geomagnetic reference field. Eos, Transactions American Geophysical Union, 86(16), 159.

Rishbeth, H. (1971). Polarization fields produced by winds in the equatorial< i> F-region. Planetary and Space Science, 19(3), 357-369.

Sastri, J. (1984). Duration of equatorial spread-F. Paper presented at the Annales Geophysicae.

Stolle, C., Lühr, H., Rother, M., & Balasis, G. (2006). Magnetic signatures of equatorial spread F as observed by the CHAMP satellite. Journal of geophysical research, 111(A2), A02304.

Downloads

Published

2013-03-30

How to Cite

Identification of Night-Time F- Region Currents from CHAMP Satellite Observations over Equatorial Africa: CHAMP Satellite Observations. (2013). International Journal of Fundamental Physical Sciences, 3(1), 9-14. https://doi.org/10.14331/ijfps.2013.330045

Issue

Section

ORIGINAL ARTICLES