- microseismic motion
- Метрология: микросейсмические колебания
Универсальный англо-русский словарь. Академик.ру. 2011.
microseismic motion
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Clapotis — Incoming wave (red) reflected at the wall produces the outgoing wave (blue), both being overlaid resulting in the clapotis (black). In hydrodynamics, the clapotis (from French: lapping of water ) is a non breaking standing wave pattern, caused… … Wikipedia
Microbarom — In acoustics, microbaroms, also known as the voice of the sea ,[1][2] are a class of atmospheric infrasonic waves generated in marine storms[3][4] by a non linear interaction of ocean surface waves with the atmosphere … Wikipedia
Microseism — In seismology, a microseism is defined as a faint earth tremor caused by natural phenomena.[1][2] The term is most commonly used to refer to the dominant background seismic noise signal on Earth, which are mostly composed of Rayleigh waves and… … Wikipedia
LIGO — For the Latvian holiday Ligo, see Jāņi.LIGO stands for Laser Interferometer Gravitational Wave Observatory. Cofounded in 1992 by Kip Thorne and Ronald Drever of Caltech and Rainer Weiss of MIT, LIGO is a joint project between scientists at MIT… … Wikipedia
Taal Volcano — Volcano Island redirects here. For the Japanese island group, see Volcano Islands. Taal Volcano Aerial photo of Taal Volcano; North is on right hand side of photo … Wikipedia
Rossi-Forel scale — The Rossi Forel scale was one of the first seismic scales to reflect earthquake intensities. Developed by Michele Stefano Conte de Rossi of Italy and François Alphonse Forel of Switzerland in the 1800s, it was used for about two decades until the … Wikipedia
Earth tide — is the sub meter motion of the Earth of about 12 hours or longer caused by Moon and Sun gravitation, also called body tide which is the largest contribution globally. The largest body tide contribution is from the semidiurnal constituents, but… … Wikipedia
