Articles | Volume 17, issue 2
https://doi.org/10.5194/tc-17-843-2023
https://doi.org/10.5194/tc-17-843-2023
Research article
 | 
20 Feb 2023
Research article |  | 20 Feb 2023

Using ice core measurements from Taylor Glacier, Antarctica, to calibrate in situ cosmogenic 14C production rates by muons

Michael N. Dyonisius, Vasilii V. Petrenko, Andrew M. Smith, Benjamin Hmiel, Peter D. Neff, Bin Yang, Quan Hua, Jochen Schmitt, Sarah A. Shackleton, Christo Buizert, Philip F. Place, James A. Menking, Ross Beaudette, Christina Harth, Michael Kalk, Heidi A. Roop, Bernhard Bereiter, Casey Armanetti, Isaac Vimont, Sylvia Englund Michel, Edward J. Brook, Jeffrey P. Severinghaus, Ray F. Weiss, and Joseph R. McConnell

Viewed

Total article views: 1,805 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,322 417 66 1,805 183 55 53
  • HTML: 1,322
  • PDF: 417
  • XML: 66
  • Total: 1,805
  • Supplement: 183
  • BibTeX: 55
  • EndNote: 53
Views and downloads (calculated since 26 Jan 2022)
Cumulative views and downloads (calculated since 26 Jan 2022)

Viewed (geographical distribution)

Total article views: 1,805 (including HTML, PDF, and XML) Thereof 1,739 with geography defined and 66 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 21 Feb 2024
Download
Short summary
Cosmic rays that enter the atmosphere produce secondary particles which react with surface minerals to produce radioactive nuclides. These nuclides are often used to constrain Earth's surface processes. However, the production rates from muons are not well constrained. We measured 14C in ice with a well-known exposure history to constrain the production rates from muons. 14C production in ice is analogous to quartz, but we obtain different production rates compared to commonly used estimates.