| Registro completo |
| Provedor de dados: |
ArchiMer
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| País: |
France
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| Título: |
An assessment of global and regional sea level for years 1993-2007 in a suite of interannual CORE-II simulations
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| Autores: |
Griffies, Stephen M.
Yin, Jianjun
Durack, Paul J.
Goddard, Paul
Bates, Susan C.
Behrens, Erik
Bentsen, Mats
Bi, Daohua
Biastoch, Arne
Boening, Claus W.
Bozec, Alexandra
Chassignet, Eric
Danabasoglu, Gokhan
Danilov, Sergey
Domingues, Catia M.
Drange, Helge
Farneti, Riccardo
Fernandez, Elodie
Greatbatch, Richard J.
Holland, David M.
Ilicak, Mehmet
Large, William G.
Lorbacher, Katja
Lu, Jianhua
Marsland, Simon J.
Mishra, Akhilesh
Nurser, A. J. George
Salas Y Melia, David
Palter, Jaime B.
Samuels, Bonita L.
Schroeter, Jens
Schwarzkopf, Franziska U.
Sidorenko, Dmitry
Treguier, Anne-marie
Tseng, Yu-heng
Tsujino, Hiroyuki
Uotila, Petteri
Valcke, Sophie
Voldoire, Aurore
Wang, Qiang
Winton, Michael
Zhang, Xuebin
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| Data: |
2014-06
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| Ano: |
2014
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| Palavras-chave: |
Sea level
CORE global ocean-ice simulations
Steric sea level
Global sea level
Ocean heat content
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| Resumo: |
The Palomares Margin, an NNE–SSW segment of the South Iberian Margin located between the Alboran and the Algerian–Balearic basins, is dissected by two major submarine canyon systems: the Gata (in the South) and the Alías–Almanzora (in the North). New swath bathymetry, side-scan sonar images, accompanied by 5 kHz and TOPAS subbottom profiles, allow us to recognize these canyons as Mediterranean examples of medium-sized turbidite systems developed in a tectonically active margin. The Gata Turbidite System is confined between residual basement seamounts and exhibits incised braided channels that feed a discrete deep-sea fan, which points to a dominantly coarse-grained turbiditic system. The Alías–Almanzora Turbidite System, larger and less confined, is a good example of nested turbiditic system within the canyon. Concentric sediment waves characterize the Alías–Almanzora deep-sea fan, and the size and acoustic character of these bedforms suggest a fine-grained turbidite system. Both canyons are deeply entrenched on a narrow continental shelf and terminate at the base of the continental slope as channels that feed deep sea fans. While the Alías–Almanzora Turbidite System is the offshore continuation of seasonal rivers, the Gata Turbidite System is exclusively formed by headward erosion along the continental slope. In both cases, left-lateral transpressive deformation influences their location, longitudinal profiles, incision at the upper sections, and canyon bending associated with specific fault segments.
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| Tipo: |
Text
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| Idioma: |
Inglês
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| Identificador: |
http://archimer.ifremer.fr/doc/00188/29904/28349.pdf
DOI:10.1016/j.ocemod.2014.03.004
http://archimer.ifremer.fr/doc/00188/29904/
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| Editor: |
Elsevier Sci Ltd
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| Relação: |
info:eu-repo/grantAgreement/EC/FP7/282672/EU//EMBRACE
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| Formato: |
application/pdf
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| Fonte: |
Ocean Modelling (1463-5003) (Elsevier Sci Ltd), 2014-06 , Vol. 78 , P. 35-89
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| Direitos: |
Published by Elsevier Ltd.
info:eu-repo/semantics/openAccess
restricted use
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