Daily Variation of the Geomagnetic Field and the Deformation of the Magnetosphere

Details Daily Variation of the Geomagnetic Field and the Deformation of the Magnetosphere Daily Variation of the Geomagnetic Field and the Deformation of the Magnetosphere

Aug 1969

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1969natur.223..603s&link_type=abstract

Nature, Volume 223, Issue 5206, pp. 603-605 (1969).

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Scientific paper

IT is well known that at low latitudes the horizontal component of the geomagnetic field has a maximum Hmax around local noon and a minimum value Hmin between 1800 and 0600 h local time. The range of the daily variation ΔH is strikingly enhanced in the region +/-3° geomagnetic latitude due to the electro jet current in the E-region. We have been interested in verifying whether at a low latitude station outside the influence of the electrojet, ΔH represents an increase on the day side over a base level at Hmin, or alternatively it is a decrease on the night side from a base level at Hmax. In the former case, we should have a positive correlation between ΔH and Hmax, with poor correlation between ΔH and Hmin. On the other hand, in the latter case, we should get a negative correlation between ΔH and Hmin and a poor correlation between ΔH and Hmax.

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