The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

A global overview of glacier advances and retreats (grouped by regions and by millennia)
for the Holocene is compiled from previous studies. The reconstructions of glacier …

We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish,
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

A prominent, abrupt climate event about 8200 years ago brought generally cold and dry
conditions to broad northern-hemisphere regions especially in wintertime, in response to a …

• The sustained rate of increase over the past century in the combined radiative forcing from
the three well-mixed greenhouse gases carbon dioxide (CO2), methane (CH4), and nitrous …

The extent of climate variability during the current interglacial period, the Holocene, is still
debated. Temperature records derived from central Greenland ice cores show one …

The causes, anatomy and consequences of the early Holocene sea level rise (EHSLR) are
reviewed. The rise, of ca 60m, took place over most of the Earth as the volume of the oceans …

During the early Holocene abrupt, decadal to centennial-scale climate variations caused
significant glacier variations in Norway. Increased freshwater inflow to the North Atlantic and …

The global temperature evolution during the Holocene is poorly known. Whereas proxy data
suggest that warm conditions prevailed in the Early to mid-Holocene with subsequent …

An integrated use of independent palaeoclimatological proxy techniques that reflect different
components of the climate system provides a potential key for functional analysis of past …