Large‐Scale Forces Under Surface Gravity Waves at a Wavy Bottom: A Mechanism for the Generation of Primary Microseisms

Fabrice Ardhuin

Open source

DOI
10.1029/2018gl078855
Published
2018-08-20
Container
Geophysical Research Letters
Publisher
American Geophysical Union (AGU)
Open access
unknown

Credibility signals

uncertain Score 64/100 under policy 1.0.0. This is a metadata assessment, not a judgment of the paper's conclusions.

Show all credibility signals

Cite this work

BibTeX

@article{allodium:10.1029/2018gl078855,
  title = {Large‐Scale Forces Under Surface Gravity Waves at a Wavy Bottom: A Mechanism for the Generation of Primary Microseisms},
  author = {Fabrice Ardhuin},
  year = {2018},
  journal = {Geophysical Research Letters},
  doi = {10.1029/2018gl078855},
  url = {https://doi.org/10.1029/2018gl078855}
}

RIS

TY  - JOUR
TI  - Large‐Scale Forces Under Surface Gravity Waves at a Wavy Bottom: A Mechanism for the Generation of Primary Microseisms
AU  - Fabrice Ardhuin
PY  - 2018
JO  - Geophysical Research Letters
DO  - 10.1029/2018gl078855
UR  - https://doi.org/10.1029/2018gl078855
ER  - 

APA

Ardhuin, F. (2018). Large‐Scale Forces Under Surface Gravity Waves at a Wavy Bottom: A Mechanism for the Generation of Primary Microseisms. Geophysical Research Letters. https://doi.org/10.1029/2018gl078855

Source records