Articles | Volume 24, issue 3
https://doi.org/10.5194/nhess-24-791-2024
https://doi.org/10.5194/nhess-24-791-2024
Research article
 | 
06 Mar 2024
Research article |  | 06 Mar 2024

Linkages between atmospheric rivers and humid heat across the United States

Colin Raymond, Anamika Shreevastava, Emily Slinskey, and Duane Waliser

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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 egusphere-2023-1219', Anonymous Referee #1, 27 Sep 2023
    • AC1: 'Reply to RC1', Colin Raymond, 11 Jan 2024
  • RC2: 'Comment on egusphere-2023-1219', Anonymous Referee #2, 29 Nov 2023
    • AC2: 'Reply to RC2', Colin Raymond, 11 Jan 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (14 Jan 2024) by Maria-Carmen Llasat
AR by Colin Raymond on behalf of the Authors (17 Jan 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (06 Feb 2024) by Maria-Carmen Llasat
AR by Colin Raymond on behalf of the Authors (07 Feb 2024)  Manuscript 
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Short summary
How can we systematically understand what causes high levels of atmospheric humidity and thus heat stress? Here we argue that atmospheric rivers can be a useful tool, based on our finding that in several US regions, atmospheric rivers and humid heat occur close together in space and time. Most typically, an atmospheric river transports moisture which heightens heat stress, with precipitation following a day later. These effects tend to be larger for stronger and more extensive systems.
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