The influence of snow sublimation and meltwater evaporation on <i>δ</i>D of water vapor in the atmospheric boundary layer of central Europe

Christner, Emanuel; Kohler, Martin; Schneider, Matthias

doi:https://doi.org/10.5194/acp-17-1207-2017

Articles | Volume 17, issue 2

https://doi.org/10.5194/acp-17-1207-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-1207-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 2

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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Final revised paper (published on 25 Jan 2017)
Supplement to the final revised paper
Preprint (discussion started on 13 Jun 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review of "The influence of snow sublimation on stable isotopes of water vapor in the atmospheric boundary layer of Central Europe"', Anonymous Referee #1, 27 Jul 2016
- AC1: 'Replies to reviewer 1', Emanuel Christner, 04 Jan 2017
RC2: 'Review #2 for Christner et al.', Anonymous Referee #2, 21 Nov 2016
- AC2: 'Replies to reviewer 2', Emanuel Christner, 04 Jan 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

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

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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.