Authors: Robert Mulvaney; Jørgen Peder Steffensen; Bo Møllesøe Vinther; Raimund Muscheler; Paul Vallelonga; Emilie Capron; Frank Wilhelms; Hubertus Fischer; Joseph R. McConnell; Thomas F. Stocker; Mirko Severi; Eliza Cook; Michael Sigl; Amaelle Landais; Sune Olander Rasmussen; Vasileios Gkinis; Sepp Kipfstuhl; Matthias Bigler; Christo Buizert; Anders Svensson; Florian Adolphi; Tobias Erhardt; Dorthe Dahl-Jensen; Helle Astrid Kjær; Frédéric Parrenin; Thomas Blunier

Venue: Climate of the Past

Type: Publication

Abstract: Abstract. The last glacial period is characterized by a number of millennial climate events that have been identified in both Greenland and Antarctic ice cores and that are abrupt in Greenland climate records. The mechanisms governing this climate variability remain a puzzle that requires a precise synchronization of ice cores from the two hemispheres to be resolved. Previously, Greenland and Antarctic ice cores have been synchronized primarily via their common records of gas concentrations or isotopes from the trapped air and via cosmogenic is... (read more)

DOI: 10.7892/boris.146005