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; OSTI
- 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
- Sponsoring Org.:
- U.S. DOE > Office of Science (SC) > Biological and Environmental Research (BER) (SC-23)
- Subject:
- 54 ENVIRONMENTAL SCIENCES; 740,000-year; Age (years before 1950 on EDC2 timescale) at bottom of averaging interval; Age (years before 1950 on EDC2 timescale) at top of averaging interval; Antarctic; Antarctica; Depth (m) at bottom of averaging interval; Depth (m) at top of averaging interval; Deuterium; Ice Core; Mean age (EDC2 timescale, mean of columns 3 and 4); TRENDS-TEMPERATURE; Temperature; dD, mean3K/permill; dD, permill; glacial
- 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:Tue Nov 30 23:00:00 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 = {Tue Nov 30 23:00:00 EST 2004},
month = {Tue Nov 30 23:00:00 EST 2004}
}
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