Document Type

Conference Proceeding

Publication Title

Annals of Glaciology

Rights and Access Note

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Publication Date

2005

First Page

77

Last Page

84

Volume Number

41

Abstract/ Summary

Shallow ice cores were obtained from widely distributed sites across the West Antarctic ice sheet, as part of the United States portion of the International Trans-Antarctic Scientific Expedition (US ITASE) program. The US ITASE cores have been dated by annual-layer counting, primarily through the identification of summer peaks in non-sea-salt sulfate (nssSO(4)(2-)) concentration. Absolute dating accuracy of better than 2 years and relative dating accuracy better than 1 year is demonstrated by the identification of multiple volcanic marker horizons in each of the cores, Tambora, Indonesia (1815), being the most prominent. Independent validation is provided by the tracing of isochronal layers from site to site using high-frequency ice-penetrating radar observations, and by the timing of mid-winter warming events in stable-isotope ratios, which demonstrate significantly better than 1 year accuracy in the last 20 years. Dating precision to 1 month is demonstrated by the occurrence of summer nitrate peaks and stable-isotope ratios in phase with nssSO(4)(2-), and winter-time sea-salt peaks out of phase, with phase variation of < 1 month. Dating precision and accuracy are uniform with depth, for at least the last 100 years.

Citation/Publisher Attribution

Steig, EJ, Mayewski, PA, Dixon, DA, Kaspari, SD, Frey, MM, Schneider, DP, Arcone, SA, et al., 2005, High-Resolution Ice Cores from Usitase (West Antarctica): Development and Validation of Chronologies and Determination of Precision and Accuracy: Annals of Glaciology, Vol 41 2005, v. 41, p. 77-84. Available on publisher's site at: http://www.ingentaconnect.com/content/igsoc/agl/2005/00000041/00000001/art00013

Publisher Statement

© Copyright 2005 by the International Glaciological Society

DOI

10.3189/172756405781813311

Version

publisher's version of the published document

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