1976
DOI: 10.1029/ja081i013p02075
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Field dependent cosmic ray streaming at high rigidities

Abstract: Data from underground µ meson telescopes at depths of 25, 40, and 80 mwe covering the period 1965–1973 have been analyzed as a function of interplanetary magnetic field direction. Cosmic ray streaming both in and perpendicular to the ecliptic plane, with directions dependent on the sense of the interplanetary magnetic field, is observed throughout the period at all depths. The field dependent streaming in the ecliptic plane exhibits some variability in amplitude and phase but contains a component in the direct… Show more

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Cited by 28 publications
(23 citation statements)
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References 10 publications
(7 reference statements)
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“…The gradient was shown to have a dependence on rigidity of P -0.6 . Swinson (1976) extended his analysis to encompass the period 1965-73 (which includes the solar polarity reversal during 1969-71). The results indicated that a south pointing (unidirectional) gradient existed across the ecliptic plane for the entire period.…”
Section: Latitudinal Density Gradientmentioning
confidence: 99%
“…The gradient was shown to have a dependence on rigidity of P -0.6 . Swinson (1976) extended his analysis to encompass the period 1965-73 (which includes the solar polarity reversal during 1969-71). The results indicated that a south pointing (unidirectional) gradient existed across the ecliptic plane for the entire period.…”
Section: Latitudinal Density Gradientmentioning
confidence: 99%
“…• The north-south anisotropy which is -distinguishable by the difference between opposite polarity is not so clearly recognized by the nucleonic intensity (Kudo and •Wada, 1977) as by the higher rigidity observation (Swinson, 1976). Plausible causes of such unclearness are contaminations by a polarity dependent effect but symmetric about the boundary, and by the boundary type Forbush decreases mentioned above.…”
Section: Resultsmentioning
confidence: 99%
“…Especially, the solar activity minimum period in the P-state seems to be a special epoch for the appearance, or the phase change, of the sidereal anisotropy, which occurs every 22 years. The occurrences of the event have been successively observed in 1954 (Conforto and Simpson, 1957), in 1975(Swinson, 1976Nagashima et al, 2010) and in 1996 (Nagashima et al, 2010).…”
mentioning
confidence: 99%
“…(Nagashima and Mori, 1976). Solid circle: Morning side (0-12 hr); Open circle: Evening side (12-24 hr); NAG, ITA, MIS and TAK (Ichinose and Murakami, 1976); EMB, SOC and BOL (Swinson, 1976); HOB (Humble and Fenton, 1975;Fenton and Fenton, 1976); CHE, HUA and CHR Forbush, 1948, 1957;Beach and Forbush, 1961 Nagashima and Mori (1976) as being due to some north-south asymmetric sidereal vectors being superposed on a common sidereal vector, in spite of the earlier find- (Nagashima et al, 1983a Fig. 6).…”
mentioning
confidence: 99%