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Detection and Modeling of Non-Tidal Oceanic Effects on the Earth's Rotation Rate

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dc.contributor.author Marcus, S. L. en_US
dc.contributor.author Chao, Y. en_US
dc.contributor.author Dickey, J. O. en_US
dc.contributor.author Gegout, P. en_US
dc.date.accessioned 2004-09-24T20:52:39Z
dc.date.available 2004-09-24T20:52:39Z
dc.date.issued 1998-05 en_US
dc.identifier.citation Science en_US
dc.identifier.citation USA en_US
dc.identifier.clearanceno 98-0790 en_US
dc.identifier.uri http://hdl.handle.net/2014/19420
dc.description.abstract Sub-decadal changes in the Earth's rotation rate, and hence in the length-of-day (LOD), are largely controlled by variations in atmospheric angular momentum. en_US
dc.format.extent 605210 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Earth's rotation heat flux oceanic angular momentum en_US
dc.title Detection and Modeling of Non-Tidal Oceanic Effects on the Earth's Rotation Rate en_US


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