We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …

Climate tip** elements are large-scale subsystems of the Earth that may transgress critical
thresholds (tip** points) under ongoing global warming, with substantial impacts on the …

Climate changes across the past 24,000 years provide key insights into Earth system
responses to external forcing. Climate model simulations, and proxy data,,,,–have …

Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

The widely accepted" Milankovitch theory" explains insolation-induced waxing and waning
of the ice sheets and their effect on the global climate on orbital timescales. In the past half …

Last Glacial millennial-scale climate variability transitioned through distinct cold stadial and
warm interstadial states. Here we use Earth system model simulations to demonstrate that …

Event stratigraphy is used to help characterise the Anthropocene as a chronostratigraphic
concept, based on analogous deep-time events, for which we provide a novel …

Specific components of the Earth system may abruptly change their state in response to
gradual changes in forcing. This possibility has attracted great scientific interest in recent …

Abrupt climate changes during the last glacial period have been detected in a global array of
palaeoclimate records, but our understanding of their absolute timing and regional …

The last glacial cycle provides the opportunity to investigate large changes in the Atlantic
Meridional Overturning Circulation (AMOC) beyond the small fluctuations evidenced from …