Articles | Volume 17, issue 2
https://doi.org/10.5194/acp-17-1207-2017
https://doi.org/10.5194/acp-17-1207-2017
Research article
 | 
25 Jan 2017
Research article |  | 25 Jan 2017

The influence of snow sublimation and meltwater evaporation on δD of water vapor in the atmospheric boundary layer of central Europe

Emanuel Christner, Martin Kohler, and Matthias Schneider

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AR by Emanuel Christner on behalf of the Authors (04 Jan 2017)  Author's response   Manuscript 
ED: Publish as is (08 Jan 2017) by Harald Saathoff
AR by Emanuel Christner on behalf of the Authors (09 Jan 2017)
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Short summary
Post-depositional fractionation of stable water isotopes due to fractioning surface evaporation introduces uncertainty to isotope applications such as the reconstruction of paleotemperatures, paleoaltimetry, and the investigation of ground water formation. In this paper we combine measurements of stable water isotopes in near-surface water vapor with a Lagrangian isotope model to investigate isotope fractionation during the evaporation of surface-layer snow in central Europe.
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