Abstract
The current rates show that there is a large region of low accumulation to the northeast of central Greenland with drops in accumulation rate of 25% 150 km, and 50% 300 km from Summit. Relatively large variations in accumulation rate over time are seen in ice cores. The resulting accumulation-rate record, which should be related to changes in local air temperature over northern Greenland, has been compared with Scandinavian tree-ring records and the data shows an early Medieval Warm Epoch, but no pronounced "Little Ice Age' and no unequivocal greenhouse warming effect as yet in northern Greenland. -from Authors
Cite
CITATION STYLE
Friedmann, A., Moore, J. C., Thorsteinsson, T., Kipfstuhl, J., & Fischer, H. (1995). A 1200 year record of accumulation from northern Greenland. Annals of Glaciology, 21, 19–25. https://doi.org/10.3189/s0260305500015548
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.