Stable water isotope behavior during the last glacial maximum: A general circulation model analysis
- 20 December 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 99 (D12) , 25791-25801
- https://doi.org/10.1029/94jd01819
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Glacial-Interglacial Changes in Moisture Sources for Greenland: Influences on the Ice Core Record of ClimateScience, 1994
- A 135,000‐year Vostok‐Specmap Common temporal frameworkPaleoceanography and Paleoclimatology, 1993
- The δ18O of atmospheric O2 from air inclusions in the Vostok Ice Core: Timing of CO2 and ice volume changes during the penultimate deglaciationPaleoceanography and Paleoclimatology, 1991
- A 250,000-Year Climatic Record from Great Basin Vein Calcite: Implications for Milankovitch TheoryScience, 1988
- Isotopic composition of atmospheric O2 in ice linked with deglaciation and global primary productivityNature, 1985
- Deuterium and oxygen-18 in European groundwaters — Links to atmospheric circulation in the pastChemical Geology: Isotope Geoscience section, 1985
- Deuterium excess in an East Antarctic ice core suggests higher relative humidity at the oceanic surface during the last glacial maximumNature, 1982
- Factors controlling stable isotope composition of European precipitationTellus, 1982
- Climatic Implications of Total Gas Content in Ice at Camp CenturyNature, 1973
- Oxygen Isotope Profiles through the Antarctic and Greenland Ice SheetsNature, 1972