Fig. 8
From: Atmospheric resonances and their coupling to vibrations of the ground and waves in the ocean
(c is adapted from (Zabotin et al. 2016).)
Bathymetry of northwest Atlantic and correlation of the oceanic and atmospheric wave activity observed in the area. a Bathymetry map of northwest Atlantic. b Probability density function of water depths in the part of the Atlantic Ocean depicted in a. Depth distribution is calculated in the area from 20° to 50° N and from 40° to 80° W using the satellite altimetry-derived global 2-min bathymetry dataset (Smith and Sandwell 1997) provided in MATLAB. The four water depths indicated by color, 150 m (yellow), 2649 m (red), 4300 m and 5900 m (white), are the depth for which the infragravity wave dispersion curves are shown in Fig. 5. c Correlation coefficient of spectral amplitudes of the wave activities observed in the Atlantic Ocean at the location of NDBC Station 44402 (39.30 °N 70.66 °W) and in the thermosphere over the Wallops Island, Virginia