A seasonal deuterium excess signal at Law Dome, coastal eastern Antarctica: A southern ocean signature
- 27 March 2000
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 105 (D6) , 7187-7197
- https://doi.org/10.1029/1999jd901085
Abstract
No abstract availableKeywords
This publication has 36 references indexed in Scilit:
- Validity of the temperature reconstruction from water isotopes in ice coresJournal of Geophysical Research: Oceans, 1997
- The climate signal in the stable isotopes of snow from Summit, Greenland: Results of comparisons with modern climate observationsJournal of Geophysical Research: Oceans, 1997
- Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transitionJournal of Geophysical Research: Oceans, 1997
- Seasonality in late-Holocene climate from ice-core recordsThe Holocene, 1997
- Calibrating the ice core paleothermometer using seasonalityJournal of Geophysical Research: Atmospheres, 1997
- A reconsideration of the initial conditions used for stable water isotope modelsJournal of Geophysical Research: Atmospheres, 1996
- Peroxide concentrations in the Dome Summit South ice core, Law Dome, AntarcticaJournal of Geophysical Research: Atmospheres, 1996
- The origin of present‐day Antarctic precipitation from surface snow deuterium excess dataJournal of Geophysical Research: Atmospheres, 1995
- Deuterium and oxygen 18 in precipitation: Isotopic model, including mixed cloud processesJournal of Geophysical Research: Atmospheres, 1994
- Antarctic climate modeling with general circulation models of the atmosphereJournal of Geophysical Research: Atmospheres, 1994