High-resolution stable isotope signature of a land-falling atmospheric river in southern Norway

Weng, Yongbiao; Johannessen, Aina; Sodemann, Harald

doi:https://doi.org/10.5194/wcd-2-713-2021

Articles | Volume 2, issue 3

https://doi.org/10.5194/wcd-2-713-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/wcd-2-713-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 2, issue 3

Research article

|

05 Aug 2021

Research article |

| 05 Aug 2021

High-resolution stable isotope signature of a land-falling atmospheric river in southern Norway

Yongbiao Weng, Aina Johannessen, and Harald Sodemann

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Final revised paper (published on 05 Aug 2021)
Supplement to the final revised paper
Preprint (discussion started on 09 Dec 2020)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review comment', Anonymous Referee #1, 24 Dec 2020
RC2: 'Wang et al.', Anonymous Referee #2, 05 Jan 2021
AC1: 'Author response on wcd-2020-58', Yongbiao Weng, 23 Feb 2021

Peer-review completion

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

AR by Yongbiao Weng on behalf of the Authors (28 Apr 2021) Author's response Author's tracked changes Manuscript

ED: Referee Nomination & Report Request started (04 May 2021) by Helen Dacre

RR by Anonymous Referee #1 (16 May 2021)

RR by Anonymous Referee #2 (20 May 2021)

ED: Publish subject to minor revisions (review by editor) (20 May 2021) by Helen Dacre

AR by Yongbiao Weng on behalf of the Authors (30 May 2021) Author's response Author's tracked changes Manuscript

ED: Publish as is (15 Jun 2021) by Helen Dacre

AR by Yongbiao Weng on behalf of the Authors (20 Jun 2021)

Short summary

High-resolution measurements of stable isotopes in near-surface vapour and precipitation show a W-shaped evolution during a 24 h land-falling atmospheric river event in southern Norway. We distinguish contributions from below-cloud processes, weather system characteristics, and moisture source conditions during different stages of the event. Rayleigh distillation models need to be expanded by additional processes to accurately predict isotopes in surface precipitation from stratiform clouds.