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Seismic Detection of Oceanic Internal Gravity Waves From Subaerial Seismometers
2021
AGU Advances
Preserved Fulltext
Oceanic internal gravity waves propagate along density stratification within the water column (Helfrich & Melville, 2006) . These waves are ubiquitous and can propagate thousands of kilometers before breaking on shoaling bathymetry and the ensuing turbulent mixing affects coastal processes, climate feedbacks, and marine ecosystems (
doi:10.1029/2021av000475
fatcat:b6j33vlhabfjtpe7tk7e6zlzoy