File Download
There are no files associated with this item.
Links for fulltext
(May Require Subscription)
- Publisher Website: 10.1111/j.1365-246X.1984.tb01920.x
- Scopus: eid_2-s2.0-0021549661
- WOS: WOS:A1984SE40500012
- Find via
Supplementary
- Citations:
- Appears in Collections:
Article: Pleistocene deglaciation and the Earth's rotation: a new analysis.
Title | Pleistocene deglaciation and the Earth's rotation: a new analysis. |
---|---|
Authors | |
Issue Date | 1984 |
Citation | Geophysical Journal - Royal Astronomical Society, 1984, v. 76 n. 3, p. 753-791 How to Cite? |
Abstract | Demonstrates 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 Identifier | http://hdl.handle.net/10722/192113 |
ISSN | 2023 Impact Factor: 2.8 2023 SCImago Journal Rankings: 1.173 |
ISI Accession Number ID |
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Wu, P | en_US |
dc.contributor.author | Peltier, WR | en_US |
dc.date.accessioned | 2013-10-23T09:26:01Z | - |
dc.date.available | 2013-10-23T09:26:01Z | - |
dc.date.issued | 1984 | en_US |
dc.identifier.citation | Geophysical Journal - Royal Astronomical Society, 1984, v. 76 n. 3, p. 753-791 | en_US |
dc.identifier.issn | 0956-540X | - |
dc.identifier.uri | http://hdl.handle.net/10722/192113 | - |
dc.description.abstract | Demonstrates 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.language | eng | en_US |
dc.relation.ispartof | Geophysical Journal - Royal Astronomical Society | en_US |
dc.title | Pleistocene deglaciation and the Earth's rotation: a new analysis. | en_US |
dc.type | Article | en_US |
dc.description.nature | link_to_OA_fulltext | - |
dc.identifier.doi | 10.1111/j.1365-246X.1984.tb01920.x | - |
dc.identifier.scopus | eid_2-s2.0-0021549661 | en_US |
dc.identifier.volume | 76 | en_US |
dc.identifier.issue | 3 | en_US |
dc.identifier.spage | 753 | en_US |
dc.identifier.epage | 791 | en_US |
dc.identifier.isi | WOS:A1984SE40500012 | - |
dc.identifier.issnl | 0956-540X | - |