Articles | Volume 23, issue 4
https://doi.org/10.5194/nhess-23-1433-2023
https://doi.org/10.5194/nhess-23-1433-2023
Research article
 | 
20 Apr 2023
Research article |  | 20 Apr 2023

The effect of deep ocean currents on ocean- bottom seismometers records

Carlos Corela, Afonso Loureiro, José Luis Duarte, Luis Matias, Tiago Rebelo, and Tiago Bartolomeu

Viewed

Total article views: 1,812 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,244 494 74 1,812 151 60 54
  • HTML: 1,244
  • PDF: 494
  • XML: 74
  • Total: 1,812
  • Supplement: 151
  • BibTeX: 60
  • EndNote: 54
Views and downloads (calculated since 12 Jul 2022)
Cumulative views and downloads (calculated since 12 Jul 2022)

Viewed (geographical distribution)

Total article views: 1,812 (including HTML, PDF, and XML) Thereof 1,744 with geography defined and 68 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
We show that ocean-bottom seismometers are controlled by bottom currents, but these are not always a function of the tidal forcing. Instead we suggest that the ocean bottom has a flow regime resulting from two possible contributions: the permanent low-frequency bottom current and the tidal current along the full tidal cycle, between neap and spring tides. In the short-period noise band the ocean current generates harmonic tremors that corrupt the dataset records.
Altmetrics
Final-revised paper
Preprint