Scientific synthesis reports and assessments
Scientific synthesis reports and assessments
SP
Articles | Volume 4-osr8
Articles | Volume 4-osr8
https://doi.org/10.5194/sp-4-osr8-11-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Report:
8th edition of the Copernicus Ocean State Report (OSR8)
https://doi.org/10.5194/sp-4-osr8-11-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 4-osr8
30 Sep 2024
 | OSR8 | Chapter 3.3
 | 30 Sep 2024 | OSR8 | Chapter 3.3

The role of air–sea heat flux for marine heatwaves in the Mediterranean Sea

Dimitra Denaxa, Gerasimos Korres, Giulia Bonino, Simona Masina, and Maria Hatzaki

Viewed

Total article views: 504 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
393 45 66 504 3 2
  • HTML: 393
  • PDF: 45
  • XML: 66
  • Total: 504
  • BibTeX: 3
  • EndNote: 2
Views and downloads (calculated since 18 Aug 2023)
Cumulative views and downloads (calculated since 18 Aug 2023)

Viewed (geographical distribution)

Total article views: 504 (including HTML, PDF, and XML) Thereof 483 with geography defined and 21 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
We investigate the air–sea heat flux during marine heatwaves (MHWs) in the Mediterranean Sea. Surface heat flux drives 44 % of the onset and only 17 % of the declining MHW phases, suggesting a key role of oceanic processes. Heat flux is more important in warmer months and onset phases, with latent heat dominating. Shorter events show a weaker heat flux contribution. In most cases, mixed layer shoaling occurs over the entire MHW duration, followed by vertical mixing after the MHW end day.
Read more
Report
8th edition of the Copernicus Ocean State Report (OSR8)
Altmetrics
Final-revised paper
Preprint