The mechanisms driving the Dansgaard-Oeschger (DO) cycles remain uncertain, but
promising hypotheses could explain it, and a comprehensive assessment of its impact is …

Paleoclimate proxies reveal abrupt transitions of the North Atlantic climate during past
glacial intervals known as Dansgaard–Oeschger (DO) events. A central feature of DO events …

Ice core records from Greenland provide evidence for multiple abrupt cold–warm–cold
events recurring at millennial time scales during the last glacial interval. Although climate …

Abstract Dansgaard‐Oeschger (D‐O) climate variability during the last glaciation was first
evidenced in ice cores and marine sediments, and is also recorded in various terrestrial …

Abstract Dansgaard–Oeschger (D–O) events, millennial-scale climate oscillations between
stadial and interstadial conditions (of up to 10–15∘ C in amplitude at high northern …

The strongest mode of centennial to millennial climate variability in the paleoclimatic record
is represented by Dansgaard–Oeschger (DO) cycles. Despite decades of research, their …

Greenland ice core records feature Dansgaard–Oeschger (D‐O) events, which are abrupt
warming episodes followed by gradual cooling during ice age climate. The three climate …

Dansgaard–Oeschger (DO) events constitute the most pronounced mode of centennial to
millennial climate variability of the last glacial period. Since their discovery, many decades of …

During the last glacial period, proxy records throughout the Northern Hemisphere document
a succession of rapid millennial-scale warming events, called Dansgaard–Oeschger (DO) …

Intermediate glacial states were characterized by large temperature changes in Greenland
and the North Atlantic, referred to as Dansgaard–Oeschger (D–O) variability, with some …