1984
DOI: 10.1007/bf01465558
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Derivation ofK-indices using magnetograms constructed from digital data

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Cited by 7 publications
(8 citation statements)
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“…98% of these low values occurred at the K = 0, 1, 2 levels. These results concur with those already obtained by Niblett et al (1984), keeping in mind the large difference in geomagnetic activity level between the two considered datasets. Basically, the downward bias leads to an underestimation of the magnetic activity during magnetic quietness while it has very limited effect during a disturbed period.…”
Section: Resultssupporting
confidence: 92%
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“…98% of these low values occurred at the K = 0, 1, 2 levels. These results concur with those already obtained by Niblett et al (1984), keeping in mind the large difference in geomagnetic activity level between the two considered datasets. Basically, the downward bias leads to an underestimation of the magnetic activity during magnetic quietness while it has very limited effect during a disturbed period.…”
Section: Resultssupporting
confidence: 92%
“…This argument concurs with that of Niblett et al (1984) who explained that "the lower K levels (...) contain much of the low energy pulsational activity with periods of 5 minutes or less". Niblett et al (1984) investigated for the OTT observatory the diurnal and seasonal distribution of the intervals for which K A and K R have different values. Their results illustrate the intervals for which K 60s   K 1s shows a local time (LT) dependency.…”
Section: Effect Of the Sampling Interval On The K Indexsupporting
confidence: 88%
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