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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 21, issue 1
Hydrol. Earth Syst. Sci., 21, 533–548, 2017
https://doi.org/10.5194/hess-21-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 21, 533–548, 2017
https://doi.org/10.5194/hess-21-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Jan 2017

Research article | 27 Jan 2017

Response of water vapour D-excess to land–atmosphere interactions in a semi-arid environment

Stephen D. Parkes et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (12 Sep 2016) by Christine Stumpp
AR by Stephen Parkes on behalf of the Authors (27 Sep 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 Oct 2016) by Christine Stumpp
RR by Anonymous Referee #1 (20 Oct 2016)
RR by Anonymous Referee #2 (24 Nov 2016)
ED: Publish subject to minor revisions (further review by Editor) (05 Dec 2016) by Christine Stumpp
AR by Stephen Parkes on behalf of the Authors (15 Dec 2016)  Author's response    Manuscript
ED: Publish as is (18 Dec 2016) by Christine Stumpp
Publications Copernicus
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Short summary
Determining atmospheric moisture sources is required for understanding the water cycle. The role of land surface fluxes is a particular source of uncertainty for moisture budgets. Water vapour isotopes have the potential to improve constraints on moisture sources. In this work relationships between water vapour isotopes and land–atmosphere exchange are studied. Results show that land surface evaporative fluxes play a minor role in the daytime water and isotope budgets in semi-arid environments.
Determining atmospheric moisture sources is required for understanding the water cycle. The role...
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