Abstract The Little Ice Age (LIA), which lasted from about 1250 to 1860 AD, was likely the
coldest period of the last 8000 years. Using new documentary data and analyses of alpine …

Abstract In the Northern Hemisphere, an insolation driven Early to Middle Holocene Thermal
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …

Two major oceanographic changes have recently propagated through several trophic levels
in coastal areas of Southeast Greenland (SEG). Firstly, the amount of drift‐ice exported from …

The Little Ice Age (LIA) was one of the coldest periods of the postglacial period in the
Northern Hemisphere. Although there is increasing evidence that this time interval was …

Understanding patterns of colonisation is important for explaining both the distribution of
single species and anticipating how ecosystems may respond to global warming. Insular …

Abstract The Atlantic Meridional Overturning Circulation (AMOC) is a key player in climate.
Here, we employ an ensemble of water hosing experiments to examine mechanisms of …

Abstract The Little Ice Age (LIA; ca. 1450–1850 CE) is the best documented cold period of
the past millennium, characterized by high-frequency volcanism, low solar activity, and high …

Frozen components on land and in the ocean (sea ice, ice sheets, glaciers and permafrost)
form the cryosphere, which, together with the ocean, moderates the physical and chemical …

The cooling transition into the Little Ice Age was the last notable shift in the climate system
prior to anthropogenic global warming. It is hypothesised that sea-ice to ocean feedbacks …

Instrumental and historic records have shown that the hydroclimatic variability on
interannual-to decadal-timescales over eastern China is spatially different, with a meridional …