1974
DOI: 10.1029/rs009i008p00757
|View full text |Cite
|
Sign up to set email alerts
|

Amplitude variation of Pc 5 pulsations at high latitudes

Abstract: Normal‐run magnetograms for the year 1967 from seven Canadian observatories were scaled to study the amplitude characteristics of Pc 5 pulsations. The results of the statistical analysis are: (1) Large amplitude Pc 5's occur in a limited region located on the poleward side of the auroral zone. (2) The diurnal variation of Pc 5 amplitude maximizes in the postnoon period at Resolute Bay and this peak tends to appear earlier and earlier in the day at the lower latitude stations, e.g., it appears in the morning at… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

2
1
0

Year Published

1975
1975
2018
2018

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 13 publications
(3 citation statements)
references
References 9 publications
2
1
0
Order By: Relevance
“…Direct ground‐based measurements of FLR frequencies support the time‐of‐flight calculations presented here, where decreased frequencies are observed during disturbed conditions (Du et al, ; Gupta, ; Warner & Orr, ). Some previous observations have been used to infer changes in the mass density distribution.…”
Section: Discussionsupporting
confidence: 82%
“…Direct ground‐based measurements of FLR frequencies support the time‐of‐flight calculations presented here, where decreased frequencies are observed during disturbed conditions (Du et al, ; Gupta, ; Warner & Orr, ). Some previous observations have been used to infer changes in the mass density distribution.…”
Section: Discussionsupporting
confidence: 82%
“…the intensity peak of Pc 5 activity on the ground occurs at latitudes of 670-75 ø in the morning sector from 0400 to 0900 LT. The amplitude of Pc 5 maximizes on the dawnside at high-latitude stations of L >• 6 [e.g.,Saito, 1964; Kokubun and Nagata, 1965;Gupta, 1974]. Thus the distribution shown inFigure 2is consistent with the statistical results of ground observations.Figure 3 compares Ogo 5 data with ground data for the L value dependence of Pc 5 period.…”
supporting
confidence: 87%
“…rence and the amphtude. These diurnal variations show a single peak in the morning at auroral latitudes, while they have two peaks in the morning and the evening at subaurorial latitudes [Saito, 1964' Hirasawa, 1970Gupta, 1974]. Hirasawa [1970] noted that Pc 5 are observed most frequently at high latitudes of 70 o to •75 ø in the morning hours in relatively quiet conditions (Kp < 2).…”
Section: Lanzerotti and Fukunishi [1974] Have Recently Reviewed The Pmentioning
confidence: 99%