1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2

We have compared the yearly production rates of 10 Be by cosmic rays in the Earths polar atmosphere over the last 50-70 years with 10 Be measurements from two separate ice cores in Greenland. These ice cores provide measurements of the annual 10 Be concentration and 10 Be flux levels during this tim...

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Main Authors: W. R. Webber, P. R. Higbie, C. W. Webber
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.4757
http://www.leif.org/EOS/1004-2675.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.380.4757 2023-05-15T16:29:29+02:00 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2 W. R. Webber P. R. Higbie C. W. Webber The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.4757 http://www.leif.org/EOS/1004-2675.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.4757 http://www.leif.org/EOS/1004-2675.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.leif.org/EOS/1004-2675.pdf text ftciteseerx 2016-09-18T00:21:41Z We have compared the yearly production rates of 10 Be by cosmic rays in the Earths polar atmosphere over the last 50-70 years with 10 Be measurements from two separate ice cores in Greenland. These ice cores provide measurements of the annual 10 Be concentration and 10 Be flux levels during this time. The scatter in the ice core yearly data vs. the production data is larger than the average solar 11 year production variations that are being measured. The cross correlation coefficients between the yearly 10 Be production and the ice core 10 Be measurements for this time period are <0.4 in all comparisons between ice core data and 10 Be production, including 10 Be concentrations, 10 Be fluxes and in comparing the two separate ice core measurements. In fact, the cross correlation between the two ice core measurements, which should be measuring the same source, is the lowest of all, only ~0.2. These values for the correlation coefficient are all indicative of a “poor ” correlation. The regression line slopes for the best fit lines between the 10 Be production and the 10 Be measurements used in the cross correlation analysis are all in the range 0.4-0.6. This is a particular problem for historical projections of solar activity based on ice core measurements which assume a 1:1 correspondence. Text Greenland ice core Unknown Greenland
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description We have compared the yearly production rates of 10 Be by cosmic rays in the Earths polar atmosphere over the last 50-70 years with 10 Be measurements from two separate ice cores in Greenland. These ice cores provide measurements of the annual 10 Be concentration and 10 Be flux levels during this time. The scatter in the ice core yearly data vs. the production data is larger than the average solar 11 year production variations that are being measured. The cross correlation coefficients between the yearly 10 Be production and the ice core 10 Be measurements for this time period are <0.4 in all comparisons between ice core data and 10 Be production, including 10 Be concentrations, 10 Be fluxes and in comparing the two separate ice core measurements. In fact, the cross correlation between the two ice core measurements, which should be measuring the same source, is the lowest of all, only ~0.2. These values for the correlation coefficient are all indicative of a “poor ” correlation. The regression line slopes for the best fit lines between the 10 Be production and the 10 Be measurements used in the cross correlation analysis are all in the range 0.4-0.6. This is a particular problem for historical projections of solar activity based on ice core measurements which assume a 1:1 correspondence.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author W. R. Webber
P. R. Higbie
C. W. Webber
spellingShingle W. R. Webber
P. R. Higbie
C. W. Webber
1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
author_facet W. R. Webber
P. R. Higbie
C. W. Webber
author_sort W. R. Webber
title 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
title_short 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
title_full 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
title_fullStr 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
title_full_unstemmed 1994 – A TROUBLING LACK OF CONCORDANCE PAPER #2
title_sort 1994 – a troubling lack of concordance paper #2
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.4757
http://www.leif.org/EOS/1004-2675.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
genre_facet Greenland
ice core
op_source http://www.leif.org/EOS/1004-2675.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.4757
http://www.leif.org/EOS/1004-2675.pdf
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