Other
Scientific paper
Jul 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.2625h&link_type=abstract
Geophysical Research Letters, Volume 28, Issue 13, p. 2625-2628
Other
4
Atmospheric Composition And Structure: Troposphere-Constituent Transport And Chemistry, Geochemistry: Isotopic Composition/Chemistry, Meteorology And Atmospheric Dynamics: Paleoclimatology
Scientific paper
Bore hole thermometry indicates that the estimated temperature shift at Summit (Greenland) from the Last Glacial to Holocene times was ~50% higher than the value obtained using the traditional isotopic δ(T) thermometer calibrated with today's data. A mechanism offered by Boyle [1997] to explain the anomalous ice core δ shift is examined. The mechanism, called the Boyle Effect, is theoretically possible but if it operated at Summit, it appears to be only capable of accounting for slightly more than half of the Summit δ18O anomaly of ~4.3%. A new semi-quantitative mechanism is proposed that could account for the remaining part of the anomaly. Other mechanisms have been advanced but they are not so amenable to quantitative application and testing.
No associations
LandOfFree
Calibration changes in the isotopic thermometer for snow according to different climatic states does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Calibration changes in the isotopic thermometer for snow according to different climatic states, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Calibration changes in the isotopic thermometer for snow according to different climatic states will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1199932