Abstract
Equipartition is a first principle in wave transport, based on the tendency of multiple scattering to homogenize phase space. We report observations of this principle for seismic waves created by earthquakes in Mexico. We find qualitative agreement with an equipartition model that accounts for mode conversions at the Earth's surface.
Highlights
Equipartition is a first principle in wave transport, based on the tendency of multiple scattering to homogenize phase space
We report observations of this principle for seismic waves created by earthquakes in Mexico
We find qualitative agreement with an equipartition model that accounts for mode conversions at the Earth’s surface
Summary
Equipartition is a first principle in wave transport, based on the tendency of multiple scattering to homogenize phase space. We find qualitative agreement with an equipartition model that accounts for mode conversions at the Earth’s surface.
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