Observations of solar-flare ionization in the mesosphere can be made using coherent-scatter radar systems. The scattered power profiles they measure in the 60-90 km altitude region is a function of the ion concentration gradient and the intensity of turbulent mixing at each altitude. By comparing the power profiles before, during and after a solar flare, it is possible to estimate the ion production rate during the flare as a function of altitude and time. This analysis is used to compare the ion production rates with generally accepted ion-chemical models. Comparisons are made with ion production rates estimated from the solar X-ray flux for the same flare made by geostationary satellites.
Observations of solar-flare ionization in the mesosphere using coherent-scatter radar
Advances in Space Research ; 4 , 4 19
01.01.1984
Sonstige
Keine Angabe
Englisch
British Library Conference Proceedings | 1997
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