Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/4361| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Stocchi, P.; Istituto di Fisica, Università degli Studi di Urbino «Carlo Bo», Urbino, Italy | en |
| dc.contributor.authorall | Spada, G.; Istituto di Fisica, Università degli Studi di Urbino «Carlo Bo», Urbino, Italy | en |
| dc.date.accessioned | 2008-11-28T08:42:39Z | en |
| dc.date.available | 2008-11-28T08:42:39Z | en |
| dc.date.issued | 2007-12 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/4361 | en |
| dc.description.abstract | Solving the sea-level equation for a spherically symmetric Earth we study the relative sea-level curves in the Mediterranean Sea in terms of Clark’s zones and we explore their sensitivity to the time-history of Late-Pleistocene ice aggregates. Since the Mediterranean is an intermediate field region with respect to the former ice sheets, glacio- and hydro-isostasy both contribute to sea-level variations throughout the Holocene. In the bulk of the basin, subsidence of the sea floor results in a monotonous sea-level rise, whereas along continental margins water loading produces the effect of «continental levering», which locally originates marked highstands followed by a sea-level fall. To describe such peculiar pattern of relative sea-level in this and other mid-latitude closed basins we introduce a new Clark’s zone (namely, Clark’s zone VII). Using a suite of publicly available ice sheet chronologies, we identify for the first time a distinct sensitivity of predictions to the Antarctic ice sheet. In particular, we show that the history of mid to Late Holocene sea-level variations along the coasts of SE Tunisia may mainly reflect the melting of Antarctica, by a consequence of a mutual cancellation of the effects from the Northern Hemisphere ice-sheets at this specific site. Ice models incorporating a delayed melting of Antarctica may account for the observations across the Mediterranean, but fail to reproduce the SE Tunisia highstand. | en |
| dc.language.iso | English | en |
| dc.relation.ispartof | Annals of Geophysics | en |
| dc.relation.ispartofseries | 6/50 (2007) | en |
| dc.subject | sea-level variations | en |
| dc.subject | glacial isostasy | en |
| dc.subject | Mediterranean Sea | en |
| dc.title | Glacio and hydro-isostasy in the Mediterranean Sea: Clark’s zones and role of remote ice sheets | en |
| dc.type | article | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.subject.INGV | 03. Hydrosphere::03.02. Hydrology::03.02.99. General or miscellaneous | en |
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| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | open | en |
| dc.contributor.author | Stocchi, P. | en |
| dc.contributor.author | Spada, G. | en |
| dc.contributor.department | Istituto di Fisica, Università degli Studi di Urbino «Carlo Bo», Urbino, Italy | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | open | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Insitute of Physics, University of Urbino, Italy | - |
| crisitem.classification.parent | 03. Hydrosphere | - |
| Appears in Collections: | Annals of Geophysics | |
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| 04stocchi.pdf | 1.58 MB | Adobe PDF | View/Open |
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