Articles | Volume 16, issue 3
https://doi.org/10.5194/amt-16-769-2023
https://doi.org/10.5194/amt-16-769-2023
Research article
 | 
09 Feb 2023
Research article |  | 09 Feb 2023

A modular field system for near-surface, vertical profiling of the atmospheric composition in harsh environments using cavity ring-down spectroscopy

Andrew W. Seidl, Harald Sodemann, and Hans Christian Steen-Larsen

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on amt-2022-208', Anonymous Referee #1, 11 Aug 2022
    • AC1: 'Reply on RC1', Andrew Walter Seidl, 24 Oct 2022
  • RC2: 'Comment on amt-2022-208', Anonymous Referee #2, 10 Sep 2022
    • AC2: 'Reply on RC2', Andrew Walter Seidl, 24 Oct 2022
  • RC3: 'Comment on amt-2022-208', Niels Munksgaard, 18 Sep 2022
    • AC3: 'Reply on RC3', Andrew Walter Seidl, 24 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Andrew Walter Seidl on behalf of the Authors (25 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (30 Nov 2022) by Maria Dolores Andrés Hernández
RR by Anonymous Referee #1 (23 Dec 2022)
ED: Publish subject to minor revisions (review by editor) (26 Dec 2022) by Maria Dolores Andrés Hernández
AR by Andrew Walter Seidl on behalf of the Authors (05 Jan 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (09 Jan 2023) by Maria Dolores Andrés Hernández
AR by Andrew Walter Seidl on behalf of the Authors (18 Jan 2023)  Manuscript 
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Short summary
It is challenging to make field measurements of stable water isotopes in the Arctic. To this end, we present a modular stable-water-isotope analyzer profiling system. The system operated for a 2-week field campaign on Svalbard during the Arctic winter. We evaluate the system’s performance and analyze any potential impact that the field conditions might have had on the isotopic measurements and the system's ability to resolve isotope gradients in the lowermost layer of the atmosphere.