We present a new gridded climate reconstruction for Europe for the last 12,000 years based
on pollen data. The reconstruction is an update of Davis et al.(2003) using the same …

Structural differences among models account for much of the uncertainty in projected climate
changes, at least until the mid-twenty-first century. Recent observations encompass too …

Climate models have continued to be developed and improved since the AR4, and many
models have been extended into Earth System models by including the representation of …

The latitudinal temperature gradient between the Equator and the poles influences
atmospheric stability, the strength of the jet stream and extratropical cyclones,–. Recent …

Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …

We analyze the global variations in the timing and magnitude of the Holocene Thermal
Maximum (HTM) and their dependence on various forcings in transient simulations covering …

The importance of reconstructing past environments quantitatively in palaeoecology is
reviewed by showing that many ecological questions asked of palaeoecological data …

In order to evaluate how much Total Solar Irradiance (TSI) has influenced Northern
Hemisphere surface air temperature trends, it is important to have reliable estimates of both …

The examination of more than 1500 paleohydrological dated records collected between 10
and 28° N during the last 50 years have been used to improve our knowledge and …

On the basis of a multi-proxy approach and a strategy combining lacustrine and marine
records along a north–south transect, data collected in the central Mediterranean within the …