摘要：As a supplementary or the only water source in dry regions, dew plays a critical role in the survival of organisms . The new hydrological tracer 17O-excess, with almost sole dependence on relative humidity, provides a new way to distinguish the evaporation processes and reconstruct the paleoclimate . Up to now, there is no published daily dew isotope record on δ2 H, δ18O, δ17O, d-excess, and 17O-excess . Here, we collected daily dew between July 2014 and April 2018 from three distinct climatic regions (i .e ., Gobabeb in the central Namib Desert with desert climate, Nice in France with Mediterranean climate, and Indianapolis in the central United States with humid continental climate) . The δ2 H, δ18O, and δ17O of dew were simultaneously analyzed using a Triple Water Vapor Isotope Analyzer based on Of-Axis Integrated Cavity Output Spectroscopy technique, and then d-excess and 17O-excess were calculated . This report presents daily dew isotope dataset under three climatic regions . It is useful for researchers to use it as a reference when studying global dew dynamics and dew formation mechanisms .
