The measurement and simulation of water vapor isotopic composition has matured rapidly
over the last decade, with long‐term data sets and comprehensive modeling capabilities …

There is large uncertainty about the magnitude of warming and how rainfall patterns will
change in response to any given scenario of future changes in atmospheric composition and …

Oxygen isotope analyses of skeletal remains (18 O/16 O, δ 18 O) are a powerful tool for
exploring major themes in bioarchaeology (the study of biological archaeological remains) …

Tropical and midlatitude precipitation is fundamentally of two types, spatially limited and
high-intensity convective or widespread and lower-intensity stratiform, owing to differences …

In this study, a first set of four present‐day global experiments with the ECHAM5
atmospheric general circulation model enhanced by stable water isotope diagnostics …

Paleoclimate observations constitute the only constraint on climate behavior prior to the
instrumental era. However, such observations only provide indirect (proxy) constraints on …

Earth's climate history is traced through the long-term covariance between the isotopic (δ
18O) composition of archived meteoric waters (groundwater, ice cores) with air temperature …

The relationship between climate variability and rainfall oxygen isotopic (δ18O) variability is
poorly constrained, especially in the tropics, where many key paleoclimate records rely on …

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 …

Abstract The European Alps and their forelands provide a range of different archives and
climate proxies for developing climate records in the time interval 60–8 thousand years (ka) …