More than a decade ago, ice core records from Greenland revealed that the last glacial
period was characterized by abrupt climate changes that recurred on millennial time scales …

The influences of a substantial weakening of the Atlantic meridional overturning circulation
(AMOC) on the tropical Pacific climate mean state, the annual cycle, and ENSO variability …

Deepwater circulation significantly changed during the last deglaciation from a shallow to a
deep-reaching overturning cell. This change went along with a drawdown of isotopically …

Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred
frequently during the last glacial period, specifically from 80–11 thousand years before …

The Atlantic meridional overturning circulation (AMOC) is a key component of the global
climate system. Recent studies suggested a twentieth‐century weakening of the AMOC of …

Using a coupled ocean–sea ice–atmosphere model of intermediate complexity, the authors
study the influence of air–sea interactions on the stability of the Atlantic Meridional …

The prevailing paradigm of abrupt climate change holds that rapid shifts associated with the
most extreme climate swings of the last glacial cycle were forced by changes in the strength …

Snowfall is an important component of Earth's climate system; however, long, continuous
high‐resolution records of global snowfall are lacking because of the absence of suitable …

Responses of the thermohaline circulation (THC) to freshwater forcing (hosing) in the
subpolar North Atlantic Ocean under present-day and the last glacial maximum (LGM) …

Abstract The North Atlantic subtropical gyre (STG) circulates warm waters between 10 and
40° N and is a potential area of heat storage during periods of reduced North Atlantic …