Now showing items 1-2 of 2
The role of the northward-directed (sub)surface limb of the Atlantic Meridional Overturning Circulation during the 8.2 ka event
(Copernicus Publications, 2014-10-24)
The so-called "8.2 ka event" is widely regarded as a major Holocene climate perturbation. It is most readily identifiable in the oxygen-isotope records from Greenland ice cores as an approximately 160-year-long cold interval ...
Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean
(Copernicus PublicationsEuropean Geosciences Union, 2010-03-30)
The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a ...