Possible solar influences on the dust profile of the GISP2 ice core from

Abstract. The Greenland Ice Sheet Project 2 (GISP2) ice core In this paper, we report and discuss the second finding and dust profile in glacial (Wisconsinan) ice from Cemral Green- demonstrate how a 22 year (Hale) dust modulation period is land has been measured using Laser-Light Scattering (LLS) g...

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Main Authors: Michael Ram, Michael R. Stolz
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1999
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.8184
http://www.leif.org/EOS/1999GL900199.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.380.8184 2023-05-15T16:30:03+02:00 Possible solar influences on the dust profile of the GISP2 ice core from Michael Ram Michael R. Stolz The Pennsylvania State University CiteSeerX Archives 1999 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.8184 http://www.leif.org/EOS/1999GL900199.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.8184 http://www.leif.org/EOS/1999GL900199.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.leif.org/EOS/1999GL900199.pdf text 1999 ftciteseerx 2016-09-18T00:22:50Z Abstract. The Greenland Ice Sheet Project 2 (GISP2) ice core In this paper, we report and discuss the second finding and dust profile in glacial (Wisconsinan) ice from Cemral Green- demonstrate how a 22 year (Hale) dust modulation period is land has been measured using Laser-Light Scattering (LLS) generated when two consecutive 11 year periods combine in a from ice. This data exhibits considerable high frequency very unique way reminiscent of the generation of a 22 year variability. By applying apprOPriate running averages to the period in the terrestrial neutron flux (Jokipii, 1991). data, certain regularities emerge. Thus, for example, when the data was smoothed with rectangular 4 and 5 year running averages, ~ 11 year dust modulations of considerable amplitude Regularities in the GISP2 Dust Profile were revealed. In this paper, we show how further smoothing of the data causes very large, longer period dust modulations The most prominem and consistera regularity in our GISP2 centered at ~91 years in a Gaussian distribution to emerge. We dust profile is the annual spring dust peaks which have been believe that this corresponds to the 80-90 year modulation of used to date the ice core with a high degree of accuracy (Ram the 11 year sunspot cycle first suggested by Gleissberg. We and Illing, 1994; Ram et al, 1995; Ram and Koenig, 1997; also show how adjacem 11 year dust periods can combine in a Meese et al., 1997). This may be viewed as a solar effect unique way to generate a 22 year (Hale) period of dust modula- inasmuch as it is the result of insolation changes at differera Text Greenland Greenland Ice Sheet Project ice core Ice Sheet Unknown Greenland Hale ENVELOPE(-86.317,-86.317,-78.067,-78.067)
institution Open Polar
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language English
description Abstract. The Greenland Ice Sheet Project 2 (GISP2) ice core In this paper, we report and discuss the second finding and dust profile in glacial (Wisconsinan) ice from Cemral Green- demonstrate how a 22 year (Hale) dust modulation period is land has been measured using Laser-Light Scattering (LLS) generated when two consecutive 11 year periods combine in a from ice. This data exhibits considerable high frequency very unique way reminiscent of the generation of a 22 year variability. By applying apprOPriate running averages to the period in the terrestrial neutron flux (Jokipii, 1991). data, certain regularities emerge. Thus, for example, when the data was smoothed with rectangular 4 and 5 year running averages, ~ 11 year dust modulations of considerable amplitude Regularities in the GISP2 Dust Profile were revealed. In this paper, we show how further smoothing of the data causes very large, longer period dust modulations The most prominem and consistera regularity in our GISP2 centered at ~91 years in a Gaussian distribution to emerge. We dust profile is the annual spring dust peaks which have been believe that this corresponds to the 80-90 year modulation of used to date the ice core with a high degree of accuracy (Ram the 11 year sunspot cycle first suggested by Gleissberg. We and Illing, 1994; Ram et al, 1995; Ram and Koenig, 1997; also show how adjacem 11 year dust periods can combine in a Meese et al., 1997). This may be viewed as a solar effect unique way to generate a 22 year (Hale) period of dust modula- inasmuch as it is the result of insolation changes at differera
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Michael Ram
Michael R. Stolz
spellingShingle Michael Ram
Michael R. Stolz
Possible solar influences on the dust profile of the GISP2 ice core from
author_facet Michael Ram
Michael R. Stolz
author_sort Michael Ram
title Possible solar influences on the dust profile of the GISP2 ice core from
title_short Possible solar influences on the dust profile of the GISP2 ice core from
title_full Possible solar influences on the dust profile of the GISP2 ice core from
title_fullStr Possible solar influences on the dust profile of the GISP2 ice core from
title_full_unstemmed Possible solar influences on the dust profile of the GISP2 ice core from
title_sort possible solar influences on the dust profile of the gisp2 ice core from
publishDate 1999
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.380.8184
http://www.leif.org/EOS/1999GL900199.pdf
long_lat ENVELOPE(-86.317,-86.317,-78.067,-78.067)
geographic Greenland
Hale
geographic_facet Greenland
Hale
genre Greenland
Greenland Ice Sheet Project
ice core
Ice Sheet
genre_facet Greenland
Greenland Ice Sheet Project
ice core
Ice Sheet
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http://www.leif.org/EOS/1999GL900199.pdf
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