METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM
Continuous recording of the intensity of the hard component of cosmic rays has been carried out at Ottawa (Geomagnetic Lat. 56.8) and at Resolute (Geomagnetic Lat. 83) in the Canadian Arctic for over a year. Two counter telescopes with different amounts of lead shielding are used at each station. Th...
Published in: | Canadian Journal of Physics |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1951
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Subjects: | |
Online Access: | https://doi.org/10.1139/p51-012 https://cdnsciencepub.com/doi/pdf/10.1139/p51-012 |
_version_ | 1821833725600595968 |
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author | Rose, D. C. |
author_facet | Rose, D. C. |
author_sort | Rose, D. C. |
collection | Canadian Science Publishing |
container_issue | 2 |
container_start_page | 97 |
container_title | Canadian Journal of Physics |
container_volume | 29 |
description | Continuous recording of the intensity of the hard component of cosmic rays has been carried out at Ottawa (Geomagnetic Lat. 56.8) and at Resolute (Geomagnetic Lat. 83) in the Canadian Arctic for over a year. Two counter telescopes with different amounts of lead shielding are used at each station. The results have been analyzed for barometer effect in four series of observations each extending over three months. When averaged, they show a barometer coefficient of –1.75% per cm. of mercury for mesons with momenta above 350 Mev./c and –2.13% per cm. of mercury for those with momenta above 630 Mev./c.A calculation has been made of the temperature and barometer effects. It was based on the variations in the probability of decay of mesons in the atmosphere, under varying atmospheric conditions. The calculations of the temperature effect do not yield results comparable with measurement; those of the barometer effect show that considerable information can be obtained about the meson spectrum from measurements of the barometer coefficients. The results favor a spectrum in agreement with parts of spectra measured by other authors. They suggest the possibility of a second maximum in the production spectrum of mesons. |
format | Article in Journal/Newspaper |
genre | Arctic |
genre_facet | Arctic |
geographic | Arctic |
geographic_facet | Arctic |
id | crcansciencepubl:10.1139/p51-012 |
institution | Open Polar |
language | English |
op_collection_id | crcansciencepubl |
op_container_end_page | 110 |
op_doi | https://doi.org/10.1139/p51-012 |
op_rights | http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_source | Canadian Journal of Physics volume 29, issue 2, page 97-110 ISSN 0008-4204 1208-6045 |
publishDate | 1951 |
publisher | Canadian Science Publishing |
record_format | openpolar |
spelling | crcansciencepubl:10.1139/p51-012 2025-01-16T20:38:56+00:00 METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM Rose, D. C. 1951 https://doi.org/10.1139/p51-012 https://cdnsciencepub.com/doi/pdf/10.1139/p51-012 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Physics volume 29, issue 2, page 97-110 ISSN 0008-4204 1208-6045 journal-article 1951 crcansciencepubl https://doi.org/10.1139/p51-012 2024-12-12T05:03:49Z Continuous recording of the intensity of the hard component of cosmic rays has been carried out at Ottawa (Geomagnetic Lat. 56.8) and at Resolute (Geomagnetic Lat. 83) in the Canadian Arctic for over a year. Two counter telescopes with different amounts of lead shielding are used at each station. The results have been analyzed for barometer effect in four series of observations each extending over three months. When averaged, they show a barometer coefficient of –1.75% per cm. of mercury for mesons with momenta above 350 Mev./c and –2.13% per cm. of mercury for those with momenta above 630 Mev./c.A calculation has been made of the temperature and barometer effects. It was based on the variations in the probability of decay of mesons in the atmosphere, under varying atmospheric conditions. The calculations of the temperature effect do not yield results comparable with measurement; those of the barometer effect show that considerable information can be obtained about the meson spectrum from measurements of the barometer coefficients. The results favor a spectrum in agreement with parts of spectra measured by other authors. They suggest the possibility of a second maximum in the production spectrum of mesons. Article in Journal/Newspaper Arctic Canadian Science Publishing Arctic Canadian Journal of Physics 29 2 97 110 |
spellingShingle | Rose, D. C. METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title | METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title_full | METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title_fullStr | METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title_full_unstemmed | METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title_short | METEOROLOGICAL EFFECTS ON COSMIC RAY INTENSITY AND THE MESON SPECTRUM |
title_sort | meteorological effects on cosmic ray intensity and the meson spectrum |
url | https://doi.org/10.1139/p51-012 https://cdnsciencepub.com/doi/pdf/10.1139/p51-012 |