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microseism's Usage Examples:

Low frequency waves (below 1 Hz) are commonly called microseisms and high frequency waves (above 1 Hz) are called microtremors.

In seismology, a microseism is defined as a faint earth tremor caused by natural phenomena.

record many things, and record many little waves, called microseisms.

generated at the ocean floor and coasts induced by ocean waves (the global microseism), to cryospheric events associated with large icebergs and glaciers.

infrasonic microbaroms into the atmosphere, and seismic signals called microseisms coupled through the ocean floor to the solid Earth.

first noticed the earth had a "pulse" also known in geology lingo as a "microseism.

They noted their similarity to microseisms observed on seismographs, and correctly hypothesized that these signals.

energy is also present as pressure oscillations at great depth, producing microseisms.

monitoring the power spectral density characteristics of ocean background microseism and Earth"s very long period hum at globally and regionally distributed.

to heavy surf on the nearby coast, an effect now called wave-generated microseism.

Algué (1856–1930), meteorologist, inventor of the barocyclometer, the nephoscope, and the microseismograph Rafael Alvarado Ballester (1924–2001) Jerónimo.

reflection of a swell at the shore, and are the source of microbaroms and microseisms.

He was able to show that "microseisms were traveling, rather than standing waves and that their origins could.