Articles | Volume 17, issue 21
https://doi.org/10.5194/gmd-17-8049-2024
https://doi.org/10.5194/gmd-17-8049-2024
Development and technical paper
 | 
12 Nov 2024
Development and technical paper |  | 12 Nov 2024

An optimal transformation method for inferring ocean tracer sources and sinks

Jan D. Zika and Taimoor Sohail

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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-2023-1220', Anonymous Referee #1, 23 Aug 2023
  • RC2: 'Comment on egusphere-2023-1220', Anonymous Referee #2, 30 Jan 2024
  • AC1: 'Response to comments on egusphere-2023-1220', Jan Zika, 23 May 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Jan Zika on behalf of the Authors (23 May 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 May 2024) by Deepak Subramani
RR by Anonymous Referee #3 (22 Jun 2024)
ED: Publish as is (09 Aug 2024) by Deepak Subramani
AR by Jan Zika on behalf of the Authors (13 Sep 2024)  Manuscript 
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Short summary
We describe a method to relate fluxes of heat and freshwater at the sea surface to the resulting distribution of seawater among categories such as warm and salty or cold and salty. The method exploits the laws that govern how heat and salt change when water mixes. The method will allow the climate community to improve estimates of how much heat the ocean is absorbing and how rainfall and evaporation are changing across the globe.