Ocean Science
Ocean Science
OS
Articles | Volume 18, issue 2
Articles | Volume 18, issue 2
https://doi.org/10.5194/os-18-523-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-18-523-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 18, issue 2
Research article
 | 
27 Apr 2022
Research article |  | 27 Apr 2022

Decomposing oceanic temperature and salinity change using ocean carbon change

Charles E. Turner, Peter J. Brown, Kevin I. C. Oliver, and Elaine L. McDonagh

Viewed

Total article views: 3,097 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,406 624 67 3,097 82 50
  • HTML: 2,406
  • PDF: 624
  • XML: 67
  • Total: 3,097
  • BibTeX: 82
  • EndNote: 50
Views and downloads (calculated since 14 Jun 2021)
Cumulative views and downloads (calculated since 14 Jun 2021)

Viewed (geographical distribution)

Total article views: 3,097 (including HTML, PDF, and XML) Thereof 2,918 with geography defined and 179 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Nov 2024
Download
Short summary
Ocean heat and carbon content increase proportionately as the planet warms. However, circulation changes in response to changing heat content, redistributing preindustrial heat, carbon, and salinity fields. Redistribution leaves properties unchanged, so we may leverage our skill identifying preindustrial carbon in order to trace preindustrial heat and salinity field redistribution. Excess salinity opposes excess-temperature-induced density change, and redistribution grows continually.
Read more