Studies consistently demonstrate that intense storms generate distinct seismic signals, known as microseisms or stormquakes, through the mechanical coupling of ocean waves with the seafloor and coastal margins.
Multiple peer-reviewed studies (e.g., [0], [2], [4], [6], [7]) document the mechanism by which intense storms, typhoons, and medicanes generate seismic waves via ocean-seafloor coupling (microseisms/stormquakes). There is no evidence in the provided literature refuting this claim.