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ABSTRACT H218O and HDO are important climatic tracers largely used to reconstruct continental palaeoclimates. The only thorough way to compare isotopic distributions in precipitation for
modern and palaeoconditions is to simulate isotope cycles using atmospheric general circulation models. H218O and HDO cycles incorporated into our atmospheric general circulation model show
good agreement between observed and predicted values for modern conditions. Access through your institution Buy or subscribe This is a preview of subscription content, access via your
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* Learn about institutional subscriptions * Read our FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS DYNAMIC AND THERMODYNAMIC INFLUENCES ON PRECIPITATION IN NORTHEAST
MEXICO ON ORBITAL TO MILLENNIAL TIMESCALES Article Open access 20 April 2023 INTERANNUAL OXYGEN ISOTOPE VARIABILITY IN INDIAN SUMMER MONSOON PRECIPITATION REFLECTS CHANGES IN MOISTURE
SOURCES Article Open access 20 May 2021 GLOBALLY COHERENT WATER CYCLE RESPONSE TO TEMPERATURE CHANGE DURING THE PAST TWO MILLENNIA Article 02 November 2023 REFERENCES * Dansgaard, W.
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Météorologie Dynamique, 24, rue Lhomond, 75231, Paris, Cedex 05, France Sylvie Joussaume & Robert Sadourny * Laboratoire de Géochimie Isotopique DPC-CEN Saclay, BP 2-91191, Gif sur
Yvette Cedex, France Jean Jouzel Authors * Sylvie Joussaume View author publications You can also search for this author inPubMed Google Scholar * Robert Sadourny View author publications
You can also search for this author inPubMed Google Scholar * Jean Jouzel View author publications You can also search for this author inPubMed Google Scholar RIGHTS AND PERMISSIONS Reprints
and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Joussaume, S., Sadourny, R. & Jouzel, J. A general circulation model of water isotope cycles in the atmosphere. _Nature_ 311, 24–29
(1984). https://doi.org/10.1038/311024a0 Download citation * Received: 22 March 1984 * Accepted: 20 June 1984 * Issue Date: 06 September 1984 * DOI: https://doi.org/10.1038/311024a0 SHARE
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