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 …

The hydrologic cycle is a fundamental component of the climate system with critical societal
and ecological relevance. Yet gaps persist in our understanding of water fluxes and their …

INTRODUCTION The uplift history of the Tibetan Plateau (TP) is critical for understanding
the evolution of the Asian monsoons and the geodynamic forces involved in collisional …

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

Local meteoric water lines (LMWLs) represent the site‐specific long‐term covariation of
hydrogen and oxygen stable isotope ratios. LMWLs have practical utility as a hydrologic …

In tropical regions, the empirical negative relationship between the isotopic content of
precipitation and rainfall amount, known as the “amount effect”, has been used as a …

We provide the first continuous measurements of isotopic composition (δD and δ18O) of
water vapor over the subtropical Eastern North Atlantic Ocean from mid‐August to mid …

Water isotope‐enabled climate and earth system models are able to directly simulate
paleoclimate proxy records to aid in climate reconstruction. A less used major advantage is …

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 …

Atmospheric Controls on Seasonal and Interannual Variations in the Precipitation Isotope in
the East Asian Monsoon Region in: Journal of Climate Volume 29 Issue 4 (2016) Jump to …