Coseismic Excitation of the Earth's Polar Motion

Gross, R.; Chao,  B.

dc.contributor.author	Gross, R.	en_US
dc.contributor.author	Chao, B.	en_US
dc.date.accessioned	2004-09-23T17:52:31Z
dc.date.available	2004-09-23T17:52:31Z
dc.date.issued	2000-03	en_US
dc.identifier.citation	Astronomical Society of the Pacific	en_US
dc.identifier.citation	USA	en_US
dc.identifier.clearanceno	00-0559	en_US
dc.identifier.uri	http://hdl.handle.net/2014/14154
dc.description.abstract	Apart from the shaking near the epicenter that is the earthquake, a seismic event creates a permanent field of dislocation in the entire Earth. This redistribution of mass changes (slightly) the Earth's interia tensor; and the Earth's rotation will change in accordance with the conservation of angular momentum.	en_US
dc.format.extent	909672 bytes
dc.format.mimetype	application/pdf
dc.language.iso	en_US
dc.subject.other	Earth Rotation polar motion earthquake	en_US
dc.title	Coseismic Excitation of the Earth's Polar Motion	en_US