We present a synchronization of the NGRIP, GRIP and GISP2 ice cores onto a master
chronology extending back to 104 ka before present, providing a consistent chronological …

Sea level change during the Quaternary is primarily a consequence of the cyclic growth and
decay of ice sheets, resulting in a complex spatial and temporal pattern. Observations of this …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

Evidence from North Atlantic deep sea cores reveals that abrupt shifts punctuated what is
conventionally thought to have been a relatively stable Holocene climate. During each of …

Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in
climate reconstructions of the Northern Hemisphere, but the oldest sections of the cores …

Deciphering the evolution of global climate from the end of the Last Glacial Maximum
approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for …

The thermal bipolar ocean seesaw hypothesis was advanced by Stocker and Johnsen
(2003) as the 'simplest possible thermodynamic model'to explain the time relationship …

Greenland ice-core records provide an exceptionally clear picture of many aspects of abrupt
climate changes, and particularly of those associated with the Younger Dryas event, as …

A prominent, abrupt climate event about 8200 years ago brought generally cold and dry
conditions to broad northern-hemisphere regions especially in wintertime, in response to a …

Oxygen isotope variations spanning the last glacial cycle and the Holocene derived from ice‐
core records for six sites in Greenland (Camp Century, Dye‐3, GRIP, GISP2, Renland and …