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Article: Pleistocene deglaciation and the Earth's rotation: a new analysis.

TitlePleistocene deglaciation and the Earth's rotation: a new analysis.
Authors
Issue Date1984
Citation
Geophysical Journal - Royal Astronomical Society, 1984, v. 76 n. 3, p. 753-791 How to Cite?
AbstractDemonstrates that two important geophysical observables may be explained as aspects of the rotational response to surface mass loading by ice sheets. These are the astronomically observed non-tidal component of the acceleration of planetary rotation and the secular drift of the rotation pole relative to the surface geography which is evident in the ILS pole path. -from Authors
Persistent Identifierhttp://hdl.handle.net/10722/192113
ISSN
2015 Impact Factor: 2.484
2015 SCImago Journal Rankings: 1.839

 

DC FieldValueLanguage
dc.contributor.authorWu, Pen_US
dc.contributor.authorPeltier, WRen_US
dc.date.accessioned2013-10-23T09:26:01Z-
dc.date.available2013-10-23T09:26:01Z-
dc.date.issued1984en_US
dc.identifier.citationGeophysical Journal - Royal Astronomical Society, 1984, v. 76 n. 3, p. 753-791en_US
dc.identifier.issn0956-540X-
dc.identifier.issn0016-8009-
dc.identifier.urihttp://hdl.handle.net/10722/192113-
dc.description.abstractDemonstrates that two important geophysical observables may be explained as aspects of the rotational response to surface mass loading by ice sheets. These are the astronomically observed non-tidal component of the acceleration of planetary rotation and the secular drift of the rotation pole relative to the surface geography which is evident in the ILS pole path. -from Authors-
dc.languageengen_US
dc.relation.ispartofGeophysical Journal - Royal Astronomical Societyen_US
dc.titlePleistocene deglaciation and the Earth's rotation: a new analysis.en_US
dc.typeArticleen_US
dc.identifier.doi10.1111/j.1365-246X.1984.tb01920.x-
dc.identifier.scopuseid_2-s2.0-0021549661en_US
dc.identifier.volume76en_US
dc.identifier.issue3en_US
dc.identifier.spage753en_US
dc.identifier.epage791en_US

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