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 …

Dansgaard–Oeschger (DO) events are a pervasive feature of glacial climates. It is widely
accepted that the associated changes in climate, which are most pronounced in the North …

While a significant influence of volcanic activity on Holocene climate is well-established, an
equally prominent role of major eruptions in the climate variability and regime shifts during …

Abstract​​​​​​​ Abrupt climate changes are defined as sudden climate changes that
took place over tens to hundreds of years or recurred at millennial timescales; they are …

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 …

This study explores the effect of southward expansion of Northern Hemisphere (American)
mid-glacial ice sheets on the global climate and the Atlantic Meridional Overturning …

Palaeoclimate time series, reflecting the state of Earth's climate in the distant past,
occasionally display very large and rapid shifts showing abrupt climate variability. The …

Dansgaard–Oeschger (DO) events occurred throughout the last glacial period. Greenland
ice cores show a rapid warming during each stadial to interstadial transition, alongside an …

Palaeoclimate time series, reflecting the state of Earth's climate in the distant past, display
occasionally very large and rapid shifts, evidencing abrupt climate variability. The …

During the last glacial period (c. 120–11 kyr BP), dramatic temperature swings, known as
Dansgaard-Oeschger (DO) events, are clearly manifest in high resolution oxygen isotope …