A High-Resolution Continuous Flow Analysis System for Polar Ice Cores-Reference-Cited by-同舟云学术

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A High-Resolution Continuous Flow Analysis System for Polar Ice Cores

Published:2016 Issue:0 Volume:34 Page:11-20
ISSN:1345-3807
Container-title:Bulletin of Glaciological Research
language:en
Short-container-title:Bulletin of Glacier Research

Author:

DALLMAYR Rémi¹,GOTO-AZUMA Kumiko¹²,ASTRID KJÆR Helle³,AZUMA Nobuhiko⁴,TAKATA Morimasa⁴,SCHÜPBACH Simon⁵⁶,HIRABAYASHI Motohiro¹

Affiliation:

1. National Institute of Polar Research

2. SOKENDAI (The Graduate University of Advanced Studies)

3. Centre for Ice and Climate, Niels Bohr Institute

4. Nagaoka University of Technology

5. Climate and Environmental Physics, Physics Institute, University of Bern

6. Present address: SBB AG

Publisher

Japanese Society of Snow and Ice

Subject

Earth-Surface Processes

Link

https://www.jstage.jst.go.jp/article/bgr/34/0/34_11/_pdf

Reference23 articles.

1. Bigler, M., Svensson, A., Kettner, E., Vallelonga, P., Nielsen, M.E. and Steffensen, J.P. (2011): Optimization of High-Resolution Continuous Flow Analysis For Transient Climate Signals in Ice Cores. Environ. Sci. Technol., 45(10), 4483-4489, doi: 10.1021/es200118j.

2. Breton, D.J., Koffman, B.G., Kurbatov, A.V., Kreutz, K.J. and Hamilton, G.S. (2012): Quantifying Signal Dispersion in a Hybrid Ice Core Melting System. Environ. Sci. Technol., 46(21), 11922-11928, doi: 10.1021/es302041k.

3. Dansgaard, W. (1964): Stable isotopes in precipitation. Tellus, 16(4), 436-468, doi: 10.1111/j.2153-3490.1964.tb00181.

4. EPICA Community Members (2004): Eight glacial cycles from an Antarctic ice core. Nature, 429(6992), 623-628, doi: 10.1038/nature02599.

5. EPICA Community Members (2006): One-to-one coupling of glacial climate variability in Greenland and Antarctica. Nature, 444(7116), 195-198, doi: 10.1038/nature05301.

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