Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

Speleothems have become a cornerstone of the approach to better understanding Earth's
climatic teleconnections due to their precise absolute chronologies, their continuous or …

Speleothem oxygen isotope records have revolutionized our understanding of the paleo
East Asian monsoon, yet there is fundamental disagreement on what they represent in terms …

An accurate and coherent chronological framework is essential for the interpretation of
climatic and environmental records obtained from deep polar ice cores. Until now, one …

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 …

The regional monsoons of the world have long been viewed as seasonal atmospheric
circulation reversal—analogous to a thermally-driven land-sea breeze on a continental …

We constructed an 800,000-year synthetic record of Greenland climate variability based on
the thermal bipolar seesaw model. Our Greenland analog reproduces much of the variability …

Here we present a new algorithm (StalAge), which is designed to construct speleothem age
models. The algorithm uses U-series ages and their corresponding age uncertainty for …

Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

Abstract The European Alps are an effective barrier for meridional moisture transport and
are thus uniquely placed to record shifts in the North Atlantic storm track pattern associated …