Physics
Scientific paper
Nov 1997
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997jastp..59.2203l&link_type=abstract
Journal of Atmospheric and Terrestrial Physics, v. 59, p. 2203-2211.
Physics
2
Scientific paper
It is now generally believed that, with the exception of auroral and higher latitudes, the F2 layer of the ionosphere is created solely by solar electromagnetic wave radiations in the UV/EUV range. This concept, however, does not appear to offer a logical explanation for the observed equinoctial maxima in planetary F2 layer ion density. It has also not been possible to produce a global-scale model of the critical frequency of the F2 layer covering a solar cycle on the basis of a single UV/EUV source. However, similar equinoctial maxima in the long-term averaged, seasonal trends of such diverse geophysical phenomena as geomagnetic activity, auroral activity, ring current intensity, planetary F2 layer ion density and the neutral thermospheric gas density are also found. The solar wind is now generally accepted to be the cause of geomagnetic activity, auroral activity and particle intensity variations within the radiation belts. Quantitative analysis of the long-term seasonal trends of these phenomena presented in this paper suggest that the solar wind may also be responsible for contributing part of the energy required for the production of the F2 layer ionization. Analysis shows that, while about 25% of the planetary ionization of the F2 layer during July may be caused by energy brought in by the solar wind, the yearly average contribution could be as high as 30% of the UV/EUV contribution, with the contribution in the equinoxes being nearly 38%. Since detailed understanding of the precise mechanism of solar wind entry into geospace is still lacking, no mechanism is suggested to show how solar wind energy is transported to the F2 layer (including low and equatorial latitudes). Magnetospheric electric fields, precipitation of energetic neutrals produced through charge exchange reactions with ions in the ring current and radiation belt particles, Joule heating, etc., may all be involved, but the energy for all such processes would still come ultimately from the solar wind. High quality F2 layer critical frequency data from all over the globe have now been available for more than half a century. Once the possibility of the impact of solar wind energy on the F2 layer ion density is recognized and established in precise quantitative terms, such a connection could become a valuable resource for advancing our understanding of solar-terrestrial relations.
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