Solar flare effects at Ebre: Regular and reversed solar flare effects, statistical analysis (1953 to 1985), a global case study and a model of elliptical ionospheric currents

Details Solar flare effects at Ebre: Regular and reversed solar flare effects, statistical analysis (1953 to 1985), a global case study and a model of elliptical ionospheric currents Solar flare effects at Ebre: Regular and reversed solar flare effects, statistical analysis (1953 to 1985), a global case study and a model of elliptical ionospheric currents

Mar 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994jgr....99.3945c&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 99, no. A3, p. 3945-3954

Physics

10

Diurnal Variations, Earth Ionosphere, Ionospheric Currents, Magnetic Effects, Solar Flares, Statistical Analysis, Solar Activity Effects, Solar Terrestrial Interactions, Sunspot Cycle

Scientific paper

This paper presents the results of the analysis of geomagnetic effects of solar flares (sfe) recorded at Ebre observatory (40.8 deg latitude N, 0.5 deg longitude E) during 33 years (1953-1985). At Ebre, located near the focused latitude, two types of sfe can be observed: regular and reversed sfe. Regular sfe are those which have phase differences less than 90 deg with the regular diurnal magnetic variation of the day, S(sub R). Reversed sfe are those which have phase differences greater than 90 deg with S(sub R). From these 33 years, 140 sfe events were selected and a statistical study was performed. We found a local time dependence of the phase differences between the sfe and S(sub R) vectors. Morning hours have slightly positive values and afternoon hours have slightly negative ones. Reversed sfe, with a phase difference exceeding 90 deg, concentrate between 10 and 12 hours. Reversed sfe show a dominant equinoctial character. Also, a weaker correlation was found between solar activity with reversed sfe (r = 0.47) than with regular sfe (r = 0.68). Using data from 67 observatories, we performed a global study of a sfe case, seen at Ebre as reversed sfe. In this case, in the northern hemisphere, the sfe system was about 1 hour of local time eastward of the S(sub R) system and formed 4 deg higher in latitude. Finally, we present a model of two elliptical ionospheric equivalent current systems with focus offset about 1 hour in local time to explain the phase difference between the sfe and S(sub q) magnetic vectors observed at Ebre. The parameters of this model have been fitted from the results of a previous statistical analysis from Ebre data. Spatial and temporal distribution of the sfe and S(sub q) vector phases are calculated with this model, and conditions for reversed sfe occurrence are predicted.

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