The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983

The annual cosmogenic 10 Be ice-core data from Dye 3 and the North Greenland Ice-core Project (NGRIP), and neutron-monitor data, 1951 – 2014, are combined to yield a record of the annual cosmic-ray intensity, 1391 – 2014. These data were then used to estimate the intensity of the heliospheric magnet...

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Published in:Solar Physics
Main Authors: McCracken, K.G., Beer, J.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Nature 2015
Subjects:
Online Access:https://doi.org/10.1007/s11207-015-0777-x
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spelling fteawag:oai:dora:eawag_8406 2023-05-15T16:03:06+02:00 The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983 McCracken, K.G. Beer, J. 2015 https://doi.org/10.1007/s11207-015-0777-x eng eng Springer Nature Solar Physics--Sol. Phys.--journals:2668--0038-0938 eawag:8406 journal id: journals:2668 issn: 0038-0938 ut: 000365220000024 local: 17858 scopus: 2-s2.0-84947493201 doi:10.1007/s11207-015-0777-x cosmogenic Be-10 solar cosmic-ray modulation solar cosmic rays interplanetary magnetic field Text Journal Article 2015 fteawag https://doi.org/10.1007/s11207-015-0777-x 2023-04-09T04:46:45Z The annual cosmogenic 10 Be ice-core data from Dye 3 and the North Greenland Ice-core Project (NGRIP), and neutron-monitor data, 1951 – 2014, are combined to yield a record of the annual cosmic-ray intensity, 1391 – 2014. These data were then used to estimate the intensity of the heliospheric magnetic field (HMF), 1391 – 1983. All of these annual data are provided in the Electronic Supplementary Material. Analysis of these annual data shows that there were significant impulsive increases in 10 Be production in the year following the very large solar cosmic-ray events of 1942, 1949, and 1956. There was an additional enhancement that we attribute to six high-altitude nuclear explosions in 1962. All of these enhancements result in underestimates of the strength of the HMF. An identification process is defined, resulting in a total of seven impulsive 10 Be events in the interval 1800 – 1942 prior to the first detection of a solar cosmic-ray event using ionization chambers. Excision of the 10 Be impulsive enhancements yields a new estimate of the HMF, designated B(PCR-2). Five of the seven 10 Be enhancements prior to 1941 are well correlated with the occurrence of very great geomagnetic storms. It is shown that a solar cosmic-ray event similar to that of 25 July 1946, and occurring in the middle of the second or third year of the solar cycle, may merge with the initial decreasing phase of the 11-year cycle in cosmic-ray intensity and be unlikely to be detected in the 10 Be data. It is concluded that the occurrence rate for solar energetic-particle (SEP) events such as that on 23 February 1956 is about seven per century, and that there is an upper limit to the size of solar cosmic-ray events. Article in Journal/Newspaper Dye 3 Dye-3 Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Greenland North Greenland Ice Core Project DORA Eawag Greenland Solar Physics 290 10 3051 3069
institution Open Polar
collection DORA Eawag
op_collection_id fteawag
language English
topic cosmogenic Be-10
solar cosmic-ray modulation
solar cosmic rays
interplanetary magnetic field
spellingShingle cosmogenic Be-10
solar cosmic-ray modulation
solar cosmic rays
interplanetary magnetic field
McCracken, K.G.
Beer, J.
The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
topic_facet cosmogenic Be-10
solar cosmic-ray modulation
solar cosmic rays
interplanetary magnetic field
description The annual cosmogenic 10 Be ice-core data from Dye 3 and the North Greenland Ice-core Project (NGRIP), and neutron-monitor data, 1951 – 2014, are combined to yield a record of the annual cosmic-ray intensity, 1391 – 2014. These data were then used to estimate the intensity of the heliospheric magnetic field (HMF), 1391 – 1983. All of these annual data are provided in the Electronic Supplementary Material. Analysis of these annual data shows that there were significant impulsive increases in 10 Be production in the year following the very large solar cosmic-ray events of 1942, 1949, and 1956. There was an additional enhancement that we attribute to six high-altitude nuclear explosions in 1962. All of these enhancements result in underestimates of the strength of the HMF. An identification process is defined, resulting in a total of seven impulsive 10 Be events in the interval 1800 – 1942 prior to the first detection of a solar cosmic-ray event using ionization chambers. Excision of the 10 Be impulsive enhancements yields a new estimate of the HMF, designated B(PCR-2). Five of the seven 10 Be enhancements prior to 1941 are well correlated with the occurrence of very great geomagnetic storms. It is shown that a solar cosmic-ray event similar to that of 25 July 1946, and occurring in the middle of the second or third year of the solar cycle, may merge with the initial decreasing phase of the 11-year cycle in cosmic-ray intensity and be unlikely to be detected in the 10 Be data. It is concluded that the occurrence rate for solar energetic-particle (SEP) events such as that on 23 February 1956 is about seven per century, and that there is an upper limit to the size of solar cosmic-ray events.
format Article in Journal/Newspaper
author McCracken, K.G.
Beer, J.
author_facet McCracken, K.G.
Beer, J.
author_sort McCracken, K.G.
title The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
title_short The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
title_full The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
title_fullStr The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
title_full_unstemmed The annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
title_sort annual cosmic-radiation intensities 1391 – 2014; the annual heliospheric magnetic field strengths 1391 – 1983, and identification of solar cosmic-ray events in the cosmogenic record 1800 – 1983
publisher Springer Nature
publishDate 2015
url https://doi.org/10.1007/s11207-015-0777-x
geographic Greenland
geographic_facet Greenland
genre Dye 3
Dye-3
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
genre_facet Dye 3
Dye-3
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
op_relation Solar Physics--Sol. Phys.--journals:2668--0038-0938
eawag:8406
journal id: journals:2668
issn: 0038-0938
ut: 000365220000024
local: 17858
scopus: 2-s2.0-84947493201
doi:10.1007/s11207-015-0777-x
op_doi https://doi.org/10.1007/s11207-015-0777-x
container_title Solar Physics
container_volume 290
container_issue 10
container_start_page 3051
op_container_end_page 3069
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