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Power spectra of infragravity waves in a deep ocean
Author(s) -
Godin Oleg A.,
Zabotin Nikolay A.,
Sheehan Anne F.,
Yang Zhaohui,
Collins John A.
Publication year - 2013
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/grl.50418
Subject(s) - spectral line , shore , geology , bathymetry , infragravity wave , spectral density , atmosphere (unit) , seafloor spreading , wind wave , seismology , meteorology , geophysics , physics , oceanography , wave propagation , optics , longitudinal wave , astronomy , mechanical wave , statistics , mathematics
Infragravity waves (IGWs) play an important role in coupling wave processes in the ocean, ice shelves, atmosphere, and the solid Earth. Due to the paucity of experimental data, little quantitative information is available about power spectra of IGWs away from the shore. Here we use continuous, yearlong records of pressure at 28 locations on the seafloor off New Zealand's South Island to investigate spectral and spatial distribution of IGW energy. Dimensional analysis of diffuse IGW fields reveals universal properties of the power spectra observed at different water depths and leads to a simple, predictive model of the IGW spectra. While sources of IGWs off New Zealand are found to have a flat power spectrum, the IGW energy density has a pronounced dependence on frequency and local water depth as a result of the interaction of the waves with varying bathymetry.