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Day to day variability in the occurrence characteristics of Sq focus during d months and its association with diurnal changes in the Declination component

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Figure

Table 1. Geographic and geomagnetic co-ordinates.
Fig. 1. Average diurnal variation of the east-west (�Y) component for theselected abnormal and normal days of the individual d-months of 1977.
Fig. 3. Variation in the �Y and �H component on an abnormal day (4February 1977) and normal day (16 February 1977) for the chain of sta-tions from equatorial (TRD) to high latitudes (NVS) in the Indo-Russianlongitude belt.
Fig. 5. Variation in the �Y and �H components on an abnormal day (1December 1977) and normal day (19 December 1977) in the dip latituderange of 0◦ to 43◦N from the equatorial (station TRD) to midlatitudes(station AAA) in the Indo-Russian longitude belt.
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