Borehole versus isotope temperatures on Greenland: Seasonality does matter
- 1 March 2000
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 27 (5) , 723-726
- https://doi.org/10.1029/1999gl006075
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Climatic controls on interannual variability of precipitation δ18O: Simulated influence of temperature, precipitation amount, and vapor source regionJournal of Geophysical Research: Atmospheres, 1999
- Water isotope module of the ECHAM atmospheric general circulation model: A study on timescales from days to several yearsJournal of Geophysical Research: Atmospheres, 1998
- Validity of the temperature reconstruction from water isotopes in ice coresJournal of Geophysical Research: Oceans, 1997
- Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transitionJournal of Geophysical Research: Oceans, 1997
- GCM analysis of local influences on ice core δ signalsGeophysical Research Letters, 1997
- Cool tropical temperatures shift the global δ18O‐T relationship: An explanation for the ice core δ18O ‐ borehole thermometry conflict?Geophysical Research Letters, 1997
- The Younger Dryas Termination and North Atlantic Deep Water Formation: Insights from climate model simulations and Greenland Ice CoresPaleoceanography and Paleoclimatology, 1997
- Seasonal Precipitation Timing and Ice Core RecordsScience, 1994
- Glacial-Interglacial Changes in Moisture Sources for Greenland: Influences on the Ice Core Record of ClimateScience, 1994
- Modeled Variations of Precipitation over the Greenland Ice SheetJournal of Climate, 1993