Physics
Scientific paper
Jul 1974
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974p%26ss...22.1139w&link_type=abstract
Planetary and Space Science, Volume 22, Issue 7, p. 1139-1143.
Physics
Scientific paper
For 4 months of synoptic records whistlers have been analyzed in two groups, high latitude (HL) whistlers with fn<=8 kHz and low latitude (LL) whistlers with fn>=8 kHz. A decrease in percentage occurrence of HL whistlers with increasing Kp is interpreted as being due to equatorwards movement of the plasmapause in the vicinity of SANAE, Antarctica (L=4). The diurnal variation in HL and LL whistler occurrence reveals an average behaviour of the plasmapause, namely, an equatorwards movement beginning at around 2000 LT followed by a return movement from 0400 LT to 0800 LT.
Clarence N. D.
Scourfield Malcolm J. W.
Woods C. A.
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