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 …

Abstract The Dansgaard-Oeschger events of the last ice age are among the best studied
abrupt climate changes, yet a comprehensive explanation is still lacking. They are most …

Atmospheric CO2 variability on the glacial–interglacial (G–IG) timescale reflects a balance
between oceanic and terrestrial processes involving carbon uptake and release. The …

To advance our understanding of the responses of tropical cyclones (TCs) to abrupt climate
transitions, we investigate the variation of genesis potential and the underlying mechanisms …

Abstract Antarctic Intermediate Water (AAIW) is an important conduit for nutrients to reach
the nutrient‐poor low‐latitude ocean areas. In the Atlantic, it forms part of the return path of …

The dynamics sha** the El Niño‐Southern Oscillation's (ENSO) response to present and
future climate change remain unclear, partly due to limited paleo‐ENSO records spanning …

Abstract Atlantic Meridional Overturning Circulation (AMOC) disruption during the last
deglaciation is hypothesized to have caused large subsurface ocean temperature …

Abrupt climate change events during glacial times have distinct tropical imprints, despite
their cause being at high latitudes. The mechanisms by which high latitudes affect low …

The occurrence of rapid last glacial temperature shifts in both Greenland ice and subpolar
marine sediment cores, so-called Dansgaard-Oeschger (DO) cycles, is evidence of a tight …

We generated a high-resolution ocean record of bottom water temperature and seawater Cd
from 546 m in the Florida Straits. The record extends to∼ 35,000 yr before present, including …