1949
DOI: 10.1103/physrev.76.1012
|View full text |Cite
|
Sign up to set email alerts
|

A Preliminary Directional Study of Cosmic Rays at High Altitude. II. Experimental Results and Interpretation

Abstract: The zenithal distribution of particles at high altitudes observed with counter telescopes has been compared with simple calculations concerning the multiplicity and angular divergence of secondary particles. The observations are in agreement with a sharply collimated forward type of production event, and disagree with the wide angle type of production of hard secondaries. The azimuthal distributions and zenithal distributions indicate a nearly isotropic primary flux, in agreement with geomagnetic consideration… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

1955
1955
1998
1998

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 14 publications
(3 citation statements)
references
References 6 publications
0
3
0
Order By: Relevance
“…Winckler and co-workers 23 found the value (0.23=b0.01)/cm 2 sec sterad for the total vertical flux under 1.9 cm Pb at 56°. Van Allen and Singer 24 found the value 0.29±0.03 above the atmosphere at 58°.…”
Section: Flux Of Primary Alpha Particlesmentioning
confidence: 93%
“…Winckler and co-workers 23 found the value (0.23=b0.01)/cm 2 sec sterad for the total vertical flux under 1.9 cm Pb at 56°. Van Allen and Singer 24 found the value 0.29±0.03 above the atmosphere at 58°.…”
Section: Flux Of Primary Alpha Particlesmentioning
confidence: 93%
“…We use the model d = d v .P(9), valid at all zenith angles. The form of P(6), as proposed by Winckler and Stroud (1949), can be derived using a standard atmospheric model for pressure o(r) = e<,exp[ -ar] as: where 8 = r-r e ,r e is the sea-level Earth radius at the telescope site and is a function of the geographic latitude of the station, r 0 -r e is the altitude of the telescope site, and a' 1 is the scaleheight of the atmosphere and equals 0.12 when b,r e and r 0 are measured in kilometres. Winckler and Stroud used the correction factor ' l ( ' ) i 0 7 ( r 0 / 2 ) cos 2 0 + 6 which is the expression for P(6) when r 0 = r e and second order terms in 5 are neglected.…”
Section: Calculating the Coupling Coefficientsmentioning
confidence: 99%
“…Atmospheric absorber depths (Winkler and Stroud 1949) and ice absorber depths were calculated for all possible counter pairs Proc.ASA6W 1985 (one counter in each wall) for a range of telescope depths in the ice. Optimization of the system depth was then achieved by firstly calculating the differential count rate response (Cooke 1975) for all the counter pairs described above and summing these to obtain several integrated responses, for various zenith angle ranges, at each system depth..…”
Section: Telescope Design and Optimizationmentioning
confidence: 99%