The stable oxygen isotope ratio (δ18O) in precipitation is an integrated tracer of atmospheric
processes worldwide. Since the 1990s, an intensive effort has been dedicated to studying …

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 …

Global climate change varies greatly in different regions, so it is necessary to
comprehensively analyze climate change in different regions through different indicators …

The deuterium excess (d) of precipitation is widely used in the reconstruction of past climatic
changes from ice cores. However, its most common interpretation as moisture source …

The assessment of sources of moisture is key to the understanding of the hydrological cycle
at different time scales, because it enables the establishment of source-sink relationships …

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 …

Raindrops interact with water vapour in ambient air while sedimenting from the cloud base
to the ground. They constantly exchange water molecules with the environment and, in sub …

We analysed contributions to run‐off using hourly stream water samples from seven
individual melt‐induced run‐off events (plus one rainfall event) during 2011, 2012 and 2013 …

Many paleoclimatic records in Southeast Asia rely on rainfall isotope ratios as proxies for
past hydroclimatic variability. However, the physical processes controlling modern rainfall …

Recent advancements in the measurement and modeling of heavy stable water isotopes (ie,
H2 18O and HDO), especially in situ and remote sensing spectroscopic vapor isotope …