The new excess term of the triple oxygen isotope composition in meteoric water, expressed
as∆′ 17 O, is conceived to track the component of kinetic fractionation in the water cycle …

Qunf Cave oxygen isotope (δ18Oc) record from southern Oman is one of the most significant
of few Holocene Indian summer monsoon cave records. However, the interpretation of the …

Recently, δ 17O and its excess (Δ′ 17O) have become increasingly significant “triple-
oxygen-isotope” indicators of distinctive hydrological processes in hydrology and …

The deuterium excess (d‐excess) of precipitation varies seasonally at sites across the globe,
an observation that has often been linked to seasonal changes in oceanic evaporation …

This Review presents the state of knowledge of the thermophysical properties of water in all
its phases and the reference formulations that provide standardized, recommended values …

The stable isotopic composition of pedogenic carbonates is central to many studies of past
climate and topography, providing a basis for our understanding of Earth's terrestrial history …

The deuterium excess (d-excess) of precipitation, which tracks kinetic fractionations during
water phase changes, has been used to trace the regions and conditions of oceanic …

The isotopic composition of precipitation is used to trace water cycling and climate change,
but interpretations of the environmental information recorded in central Andean precipitation …

Speleothem oxygen isotope (δ 18 O) records provide key insight into the rate and timing of
terrestrial paleoclimate changes during the late Quaternary. However, it can be difficult to …

Triple oxygen isotope ratios (∆′ 17O) offer new opportunities to improve reconstructions of
past climate by quantifying evaporation, relative humidity, and diagenesis in geologic …