Hostname: page-component-745bb68f8f-lrblm Total loading time: 0 Render date: 2025-02-08T22:19:12.247Z Has data issue: false hasContentIssue false
  • English
  • Français

Core handling, transportation and processing for the South Pole ice core (SPICEcore) project — ERRATUM

Published online by Cambridge University Press:  17 September 2021

Joseph M. Souney ,
Mark S. Twickler ,
Murat Aydin ,
Eric J. Steig ,
T. J. Fudge ,
Leah V. Street ,
Melinda R. Nicewonger ,
Emma C. Kahle ,
Jay A. Johnson  and
Tanner W. Kuhl
...Show all authors
Joseph M. Souney
Affiliation:
Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA
Mark S. Twickler
Affiliation:
Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH, USA
Murat Aydin
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, CA, USA
Eric J. Steig
Affiliation:
Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA
T. J. Fudge
Affiliation:
Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA
Leah V. Street
Affiliation:
Antarctic Support Contract, U.S. Antarctic Program, Denver, CO, USA
Melinda R. Nicewonger
Affiliation:
Department of Earth System Science, University of California Irvine, Irvine, CA, USA
Emma C. Kahle
Affiliation:
Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA
Jay A. Johnson
Affiliation:
U.S. Ice Drilling Program, University of Wisconsin-Madison, Madison, WI, USA
Tanner W. Kuhl
Affiliation:
U.S. Ice Drilling Program, University of Wisconsin-Madison, Madison, WI, USA
Kimberly A. Casey
Affiliation:
National Land Imaging Program, U.S. Geological Survey, Reston, VA, USA Earth Sciences Division, NASA Goddard Space Flight Center, Greenbelt, MD, USA
John M. Fegyveresi
Affiliation:
School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ, USA
Richard M. Nunn
Affiliation:
NSF-Ice Core Facility, U.S. Geological Survey, Denver, CO, USA
Geoffrey M. Hargreaves
Affiliation:
NSF-Ice Core Facility, U.S. Geological Survey, Denver, CO, USA
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Erratum
Information
Annals of Glaciology , Volume 62 , Issue 85-86 , September 2021 , pp. 391
Check for updates
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press

A corrected version of Figure 12 is provided here. The updated figure has several erroneous labels removed

Fig. 12. Cross-section of the 98 mm diameter ice core showing the generalized cut plan used at the NSF-ICF during the (a) 2015 CPL (5–555 m depth) and the (b) 2016 and 2017 CPLs (555–1751 m depth). After the 2015 CPL, the cut plan was modified to provide two equal-area sticks for water stable-isotope analysis (Iso). Over 10 300 samples have been cut to date and distributed to 16 individually funded investigators from 13 US institutions for analysis. The thick red line represents the ice removed by the planer before the electrical properties are measured on the core. Chem = chemistry; Iso = water stable isotopes; Be10 = beryllium-10; Phys Prop = physical properties.

Footnotes

*

Present address: NOAA ESRL Global Monitoring Division, Boulder, CO, USA.

Figure 0

Fig. 12. Cross-section of the 98 mm diameter ice core showing the generalized cut plan used at the NSF-ICF during the (a) 2015 CPL (5–555 m depth) and the (b) 2016 and 2017 CPLs (555–1751 m depth). After the 2015 CPL, the cut plan was modified to provide two equal-area sticks for water stable-isotope analysis (Iso). Over 10 300 samples have been cut to date and distributed to 16 individually funded investigators from 13 US institutions for analysis. The thick red line represents the ice removed by the planer before the electrical properties are measured on the core. Chem = chemistry; Iso = water stable isotopes; Be10 = beryllium-10; Phys Prop = physical properties.