Abrupt changes in climate have occurred in many locations around the globe over the last
glacial cycle, with pronounced temperature swings on timescales of decades or less in the …

Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

We use numerical climate simulations, paleoclimate data, and modern observations to study
the effect of growing ice melt from Antarctica and Greenland. Meltwater tends to stabilize the …

X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …

Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial
climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet …

Dansgaard‐Oeschger (D‐O) cycles are the most dramatic, frequent, and wide‐reaching
abrupt climate changes in the geologic record. On Greenland, D‐O cycles are characterized …

Sea surface temperatures (SSTs) recorded by alkenones and oxygen isotopes in the
Alboran basin are used here to describe, at an unprecedented fine temporal resolution, the …

Climatic variabilities on millennial and longer time scales with a bipolar seesaw pattern have
been documented in paleoclimatic records, but their frequencies, relationships with mean …

The last glacial interval experienced abrupt climatic changes called Dansgaard–Oeschger
(DO) events. These events manifest themselves as rapid increases followed by slow …

Ocean-induced ice-shelf melt is one of the largest uncertainty factors in the Antarctic
contribution to future sea-level rise. Several parameterisations exist, linking oceanic …