Articles | Volume 21, issue 14
Atmos. Chem. Phys., 21, 10911–10937, 2021
https://doi.org/10.5194/acp-21-10911-2021
Atmos. Chem. Phys., 21, 10911–10937, 2021
https://doi.org/10.5194/acp-21-10911-2021
Research article
20 Jul 2021
Research article | 20 Jul 2021

Experimental investigation of the stable water isotope distribution in an Alpine lake environment (L-WAIVE)

Patrick Chazette et al.

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Interactive discussion

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
AR by Patrick Chazette on behalf of the Authors (29 Mar 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (31 Mar 2021) by Heini Wernli
RR by Anonymous Referee #1 (14 Apr 2021)
ED: Reconsider after major revisions (29 Apr 2021) by Heini Wernli
AR by Patrick Chazette on behalf of the Authors (08 May 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (19 May 2021) by Heini Wernli
RR by Anonymous Referee #1 (10 Jun 2021)
ED: Publish subject to technical corrections (11 Jun 2021) by Heini Wernli
AR by Patrick Chazette on behalf of the Authors (14 Jun 2021)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Patrick Chazette on behalf of the Authors (08 Jul 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (19 Jul 2021) by Heini Wernli
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Short summary
To gain understanding on the vertical structure of atmospheric water vapour above mountain lakes and to assess its link to the isotopic composition of the lake water and small-scale dynamics, the L-WAIVE field campaign was conducted in the Annecy valley in the French Alps in June 2019. Based on a synergy between ground-based, boat-borne, and airborne measuring platforms, significant gradients of isotopic content have been revealed at the transitions to the lake and to the free troposphere.
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