Hundreds of coral paleoclimate records have been developed over the past several
decades, significantly extending the instrumental record and improving our understanding of …

The analysis of hydrogen (δD) and oxygen (δ18O) isotope ratios of H2O are widely used
tools for studies of the hydrological cycle (Friedman 1953; Dansgaard 1954; Gonfiantini …

Climate trends in the Antarctic region remain poorly characterized, owing to the brevity and
scarcity of direct climate observations and the large magnitude of interannual to decadal …

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 …

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 …

We present here the first results, for the preindustrial and mid-Holocene climatological
periods, of the newly developed isotope-enhanced version of the fully coupled Earth system …

Long‐term continuous monitoring of water vapor isotopes has great potential to improve our
understanding of mechanisms that control stable isotope variations in hydrological …

Surface processes in high latitudes play an important role in global climate and thus
understanding the physics of these systems is critical for improving climate projections. The …

The hydrogen and oxygen isotopic composition of ice cores from Summit, Greenland, has
provided invaluable information about variations in past climate. However, interpretations of …

Surface processes alter the water stable isotope signal of the surface snow after deposition.
However, it remains an open question to which extent surface post‐depositional processes …