On deglaciation induced perturbations of the geoid

dc.contributor.author	Wolf, Detlef	de
dc.date.accessioned	2010-02-08	de
dc.date.accessioned	2016-03-31T11:42:02Z
dc.date.available	2010-02-08	de
dc.date.available	2016-03-31T11:42:02Z
dc.date.issued	1986	de
dc.description.abstract	The importance of geoid perturbations in interpreting tilts of glacial lake levels is investigated, using a representative theoretical model. It is shown that near the ice margin, the slope of the Earth's perturbed surface is everywhere large compared with the slope of the associated undulation of the geoid. Perturbations of the geoid may therefore be neglected in interpretations of glacial strandline tilt.	en
dc.identifier.other	321599918	de
dc.identifier.uri	http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50817	de
dc.identifier.uri	http://elib.uni-stuttgart.de/handle/11682/7146
dc.identifier.uri	http://dx.doi.org/10.18419/opus-7129
dc.language.iso	en	de
dc.rights	info:eu-repo/semantics/openAccess	de
dc.subject.classification	Ablation <Geographie> , Geoid	de
dc.subject.ddc	550	de
dc.title	On deglaciation induced perturbations of the geoid	en
dc.type	article	de
ubs.fakultaet	Fakultätsübergreifend / Sonstige Einrichtung	de
ubs.institut	Sonstige Einrichtung	de
ubs.opusid	5081	de
ubs.publikation.source	Journal of Earth Sciences 23 (1986), S. 269-272	de
ubs.publikation.typ	Zeitschriftenartikel	de

Files

Now showing 1 - 1 of 1

Now showing 1 - 1 of 1