Greenland ice core evidence for spatial and temporal variability of the Atlantic Multidecadal Oscillation
[1] The Greenland d18O ice core record is used as a proxy for Greenland surface air temperatures and to interpret Atlantic Multidecadal Oscillation (AMO) variability. An analysis of annual d18O data from six Arctic ice cores (five from Greenland and one from Canada’s Ellesmere Island) suggests a sig...
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Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.640.8540 http://www.leif.org/EOS/2012GL051241.pdf |