Geomagnetic control of the midlatitude foF1 and foF2 long-term variations: Recent observations in Europe

A new very simple method, allowing an easy control, has been applied to extract long-term (11year) f(o)F(211y) and f(o)F(111y) variations from June f(o)F(2) and f(o)F(1) monthly median observations at European Slough/Chilton and Juliusruh stations, including recent data until 2015. The aim of the analysis was to check the validity of the geomagnetic control of f(o)F(2) and f(o)F(1) long-term variations in the 21st century with the main accent on the period including the last deep solar minimum in 2008-2009. The geomagnetic control was shown to be valid. Moreover, the dependence on geomagnetic activity has become more pronounced and explicit after 1990. A simultaneous analysis of f(o)F(2) and f(o)F(1) long-term variations improves the reliability of the obtained conclusions and helps understand the physical mechanism of these variations. Due to common neutral composition and the similarity of photochemical processes noontime f(o)F(2) and f(o)F(1) demonstrate similar long-term variations: the correlation coefficient between foF(211y) and f(o)F(111y) is 0.834 at Slough/Chilton and 0.884 at Juliusruh with the 99% confidence level according to Fisher's F criterion. Midnight long-term f(o)F(211y) variations also manifest a pronounced dependence on Ap(11y) which may be interpreted in the framework of the geomagnetic control concept.