1998
DOI: 10.1023/a:1005022907102
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Cited by 34 publications
(16 citation statements)
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“…ae We consider 26-day variations in the cosmic rays, which are seen up to the highest latitudes observed by Ulysses. This unexpected observation places important constraints on the ability of and the mechanism by which particles are transported in latitude (see also Simpson, 1998). The conclusions of these sections and their implications for our assessment of the global processes which control cosmic ray modulation are summarized in the final section.…”
Section: Introductionmentioning
confidence: 90%
“…ae We consider 26-day variations in the cosmic rays, which are seen up to the highest latitudes observed by Ulysses. This unexpected observation places important constraints on the ability of and the mechanism by which particles are transported in latitude (see also Simpson, 1998). The conclusions of these sections and their implications for our assessment of the global processes which control cosmic ray modulation are summarized in the final section.…”
Section: Introductionmentioning
confidence: 90%
“…Note that such recurrent GCR decreases during HSSs represent the well known 27 day variations (Fonger 1953;Simpson 1998). The intensity then recovered completely or partially, mostly before the trailing edge of the stream.…”
Section: Trains and Recurrent Trains Of Enhanced And Suppressed Diurnmentioning
confidence: 61%
“…Thus corotational variations in solar wind speed are associated with well-known "synodic" or "27 day variations" in the GCR flux (Fonger 1953;Simpson 1998;da Silva et al 2007), which have sometimes been called "recurrent Forbush decreases." An HSS causes a temporary cosmic ray decrease, either due to shielding by the CIR (Heber et al 1999;Richardson 2004) or due to a change in particle diffusion properties in local interplanetary space in low and middle heliolatitudes (Chih & Lee 1986;Kóta & Jokipii 1991).…”
Section: Introductionmentioning
confidence: 99%
“…The GCR flux depressions appear associated with those periods of time during which the solar wind plasma speed (V ) is >400 km s −1 and/or the IMF intensity (B) is >10 nT (second and fourth panels in Figure 6). This scenario basically corresponds to the passage of high-speed solar wind streams and/or CIRs (Harang 1968;Storini 1990;Cane et al 1995;Simpson 1998;McKibben et al 1999;Bazilevskaya 2000). When GCR short-term variations are correlated with the BV parameter, the role of the magnetic field trend is privileged with respect to that of the solar wind speed as the IMF variations are larger than those of the solar wind speed.…”
Section: Observations Of Gcr Flux Short-term Variations Aboard Lpfmentioning
confidence: 99%