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dc.contributor.authorKjenstad, Kjell
dc.date.accessioned2007-01-10T12:05:42Z
dc.date.accessioned2017-04-19T12:28:45Z
dc.date.available2007-01-10T12:05:42Z
dc.date.available2017-04-19T12:28:45Z
dc.date.issued1997
dc.identifier.citationNorsk geografisk tidsskrift 51 (1997), p. 29-34
dc.identifier.issn0029-1951
dc.identifier.urihttp://hdl.handle.net/11250/2438091
dc.description.abstractThe model is represented by a four-dimensional trend function giving the elevation of the sea level (Z) above the present one as a function of locality co-ordinates (x and y) and time co-ordinate (t). The function and an estimate of its uncertainty have been given compact mathematical formulation by means of matrix representation. This paper only presents the model it does not apply it. No comparisons with other models are made. The model has previously been tested on data from the Oslofjord area, where it has been applied to reconstruction of the ice-front recession chronology.
dc.format.extent88301 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherTaylor & Francis
dc.subjectModeling
dc.subjectQuaternary geology
dc.titleA four-dimensional time-space trend model to be applied in the reconstruction of former sea levels and ice-front recession
dc.typeJournal article
dc.typePeer reviewed
dc.subject.nsi555
dc.subject.nsi415
dc.subject.nsi465


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