INTERNATIONAL JOURNAL OF GEOMAGNETISM AND AERONOMY VOL. 5, GI3001, doi:10.1029/2004GI000071, 2005

2. Data Analysis

[3]  The morphological analysis was made for Huancayo ( j = 12.0 oS; l = 284.7 oE; I=1.3 ) and Kodaikanal ( j = 10.2 oN; l = 77.5 oW; I=2.6 ) over all available years of observations, (1957-1989) and (1957-1987) for the two stations, respectively. Following to the method by MDL a 27-day NmF2 running median centered to the day in question rather than usual monthly median was used for the Q disturbances analysis. The advantages of using the 27-day median were discussed by MDL. In our analysis, Q disturbances were referred to hourly ( NmF2/NmF2 med -1 ) deviations more than 40% if all 3-hour ap indices were le 7 for 24 previous hours. Normally, this provides a selection of quiet time periods (MDL). Three levels of solar activity were considered using 12-month running mean sunspot number: solar minimum R12 < 50, medium R12 = 50-100, and maximum R12 > 100.



AGU

Citation: Depueva, A. Kh., A. V. Mikhailov, and V. Kh. Depuev (2005), Quiet time F2-layer disturbances at geomagnetic equator, Int. J. Geomagn. Aeron., 5, GI3001, doi:10.1029/2004GI000071.

Copyright 2005 by the American Geophysical Union

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