Dominant influence of atmospheric circulation on snow accumulation in Greenland over the past 18,000 years
- 1 January 1995
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 373 (6509) , 52-54
- https://doi.org/10.1038/373052a0
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- Calibration of the δ18O isotopic paleothermometer for central Greenland, using borehole temperaturesJournal of Glaciology, 1994
- Electrical conductivity measurements from the GISP2 and GRIP Greenland ice coresNature, 1993
- Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice coresNature, 1993
- Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas eventNature, 1993
- Toward using borehole temperatures to calibrate an isotopic paleothermometer in central GreenlandPalaeogeography, Palaeoclimatology, Palaeoecology, 1992
- Implications for climate and sea level of revised IPCC emissions scenariosNature, 1992
- Ice-core dating and chemistry by direct-current electrical conductivityJournal of Glaciology, 1992
- Predicted time-scales for GISP2 and GRIP boreholes at Summit, GreenlandJournal of Glaciology, 1992
- POLAR ICE CORES AND CLIMATE HISTORYWeather, 1991
- The mass balance of the Greenland ice sheet: sensitivity to climate change as revealed by energy-balance modellingThe Holocene, 1991