Evidence for substantial accumulation rate variability in Antarctica during the Holocene through synchronization of CO2 in the Taylor Dome , Dome C and DML ice cores

hdl:10013/epic.20385

publisher:10.1016/j.epsl.2004.05.007

Evidence for substantial accumulation rate variability in Antarctica during the Holocene through synchronization of CO2 in the Taylor Dome , Dome C and DML ice cores

Monnin, E., Steig, E. J., Siegenthaler, U., Kawamura, K., Schwander, J., Stauffer, B., Stocker, T. F., Morse, D. L., Barnola, J. M., Bellier, B., Raynaud, D. and Fischer, Hubertus ;

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hufischer [ at ] awi-bremerhaven.de

Abstract

Item Type

Article

Authors

Monnin, E., Steig, E. J., Siegenthaler, U., Kawamura, K., Schwander, J., Stauffer, B., Stocker, T. F., Morse, D. L., Barnola, J. M., Bellier, B., Raynaud, D. and Fischer, Hubertus ;

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AWI Organizations > Geosciences > Glaciology

Programs

Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Helmholtz Research Programs > MARCOPOLI (2004-2008) > New Themes
Helmholtz Research Programs > MARCOPOLI (2004-2008) > NEW KEYS - New keys to polar climate archives

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Published

Eprint ID

9889

DOI 10.1016/j.epsl.2004.05.007

Cite as

Monnin, E. , Steig, E. J. , Siegenthaler, U. , Kawamura, K. , Schwander, J. , Stauffer, B. , Stocker, T. F. , Morse, D. L. , Barnola, J. M. , Bellier, B. , Raynaud, D. and Fischer, H. (2004): Evidence for substantial accumulation rate variability in Antarctica during the Holocene through synchronization of CO2 in the Taylor Dome , Dome C and DML ice cores , Earth and planetary science letters, 224 , pp. 45-54 . doi: 10.1016/j.epsl.2004.05.007

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hdl:10013/epic.20385.d001

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