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Citation:
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
Cite this page as:
hdl:10013/epic.20385
DOI:
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Supplementary Information:
Abstract:
Further Details:
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.
;
Fischer, Hubertus
Divisions:
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
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
Eprint ID:
9889


