Abstract The Greater Yellowstone Glacial System (GYGS) covered about 20,000 km 2 at its
maximum Pleistocene extent. The initiation, culmination, and ultimate decay of the GYGS …

While the climate evolution of North America during the last deglaciation has received
considerable attention, few detailed model–data comparisons of the deglacial hydroclimate …

The climatic controls on the stable carbon isotopic composition (δ 13 C) of speleothem
carbonate are less often discussed in the scientific literature in contrast to the frequently …

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 complicity of long-term land surface temperature (LST) changes has been under
investigated and less understood, hindering our understanding of the history and …

Stable isotope records from speleothems provide information on past climate changes, most
particularly information that can be used to reconstruct past changes in precipitation and …

In recent decades speleothems have become valuable climate archives and are of crucial
importance for the investigation of past climate conditions. Albeit much progress has been …

This book is an unorthodox ground-breaking scientific study on natural climate change and
its contribution to ongoing multi-centennial global warming. The book critically reviews the …

Quaternary climate changes are driven in part by variations in the distribution and strength of
insolation due to orbital parameters. Continental climate variability is well documented for …

Surface exposure dating with terrestrial cosmogenic nuclides (TCNs) has become the
primary method for determining numerical ages of Pleistocene mountain glacial deposits …