The Earth is regularly emitting a low frequency 'hum' equivalent to the energy released from a magnitude 5.75 earthquake. Since its discovery the source of this 'noise' has been projected to be some combination of the interactions between the atmosphere, the oceans and solid Earth, but exactly what produces it has remained something of a mystery. Now Spahr Webb presents calculations that suggest that seismic energy generated by the interaction of ocean waves with the shallow continental shelves, rather than atmospheric turbulence, is the probable source of the hum.
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Department of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong UniversityDepartment of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong University
Xi Zhao
Hua Liu
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Department of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong UniversityDepartment of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong University
Hua Liu
Benlong Wang
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Department of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong UniversityDepartment of Engineering Mechanics,MOE Key Laboratory of Hydrodynamics,Shanghai Jiao Tong University
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Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USAUniv Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
Uchiyama, Yusuke
McWilliams, James C.
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Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USAUniv Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
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Virginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USAVirginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USA
Wright, L. D.
Friedrichs, C. T.
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Virginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USAVirginia Inst Marine Sci, Coll William & Mary, Gloucester Point, VA 23062 USA