740,000-year Deuterium Record in an Ice Core from Dome C, Antarctica
Abstract
Because isotopic fractions of the heavier oxygen-18 (18O) and deuterium (2H) in snowfall are temperature-dependent and a strong spatial correlation exists between the annual mean temperature and the mean isotopic fraction of 18O or 2H in precipitation, it is possible to derive temperature records from the records of those isotopes in ice cores.For access to the data files, click this link to the CDIAC data transition website: http://cdiac.ess-dive.lbl.gov/trends/temp/domec/domec.html
- Authors:
-
- Institut Pierre Simon Laplace, Laboratoire des Sciences du Climat et de l'Environnement UMR CEA-CNRS
- Publication Date:
- Other Number(s):
- doi:10.3334/CDIAC/CLI.007; cdiac:doi 10.3334/CDIAC/cli.007
- Research Org.:
- Environmental System Science Data Infrastructure for a Virtual Ecosystem (ESS-DIVE) (United States)
- Sponsoring Org.:
- U.S. DOE > Office of Science (SC) > Biological and Environmental Research (BER) (SC-23)
- Subject:
- 54 ENVIRONMENTAL SCIENCES
- Keywords:
- Antarctic; Temperature; Antarctica; Deuterium; glacial; Ice Core; 740,000-year; TRENDS-TEMPERATURE; Depth (m) at top of averaging interval; Depth (m) at bottom of averaging interval; Age (years before 1950 on EDC2 timescale) at top of averaging interval; Age (years before 1950 on EDC2 timescale) at bottom of averaging interval; Mean age (EDC2 timescale, mean of columns 3 and 4) ; dD, permill; dD, mean3K/permill
- OSTI Identifier:
- 1394914
- DOI:
- https://doi.org/10.3334/CDIAC/cli.007
Citation Formats
Jouzel, J. 740,000-year Deuterium Record in an Ice Core from Dome C, Antarctica. United States: N. p., 2004.
Web. doi:10.3334/CDIAC/cli.007.
Jouzel, J. 740,000-year Deuterium Record in an Ice Core from Dome C, Antarctica. United States. doi:https://doi.org/10.3334/CDIAC/cli.007
Jouzel, J. 2004.
"740,000-year Deuterium Record in an Ice Core from Dome C, Antarctica". United States. doi:https://doi.org/10.3334/CDIAC/cli.007. https://www.osti.gov/servlets/purl/1394914. Pub date:Wed Dec 01 00:00:00 EST 2004
@article{osti_1394914,
title = {740,000-year Deuterium Record in an Ice Core from Dome C, Antarctica},
author = {Jouzel, J.},
abstractNote = {Because isotopic fractions of the heavier oxygen-18 (18O) and deuterium (2H) in snowfall are temperature-dependent and a strong spatial correlation exists between the annual mean temperature and the mean isotopic fraction of 18O or 2H in precipitation, it is possible to derive temperature records from the records of those isotopes in ice cores.For access to the data files, click this link to the CDIAC data transition website: http://cdiac.ess-dive.lbl.gov/trends/temp/domec/domec.html},
doi = {10.3334/CDIAC/cli.007},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Dec 01 00:00:00 EST 2004},
month = {Wed Dec 01 00:00:00 EST 2004}
}
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Works referencing / citing this record:
Ocean carbon cycling during the past 130 000 years – a pilot study on inverse palaeoclimate record modelling
journal, January 2016
- Heinze, Christoph; Hoogakker, Babette A. A.; Winguth, Arne
- Climate of the Past, Vol. 12, Issue 10