FN Archimer Export Format
PT J
TI An assessment of global and regional sea level for years 1993-2007 in a suite of interannual CORE-II simulations
BT 
AF 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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C1 NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540, USA.
   Univ Arizona, Dept Geosci, Tucson, AZ 85721, USA.
   Lawrence Livermore Natl Lab, Program Climate Model Diag & Intercomparison, Livermore, CA, USA.
   Natl Ctr Atmospher Res, Boulder, CO 80307, USA.
   GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany.
   Uni Res Ltd, Uni Climate, Bergen, Norway.
   CSIRO, Ctr Australian Weather & Climate Res, Melbourne, Vic, Australia.
   Florida State Univ, Ctr Ocean Atmospher Predict Studies, Tallahassee, FL 32306, USA.
   Alfred Wegener Inst AWI Polar & Marine Res, Bremerhaven, Germany.
   Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas, Australia.
   Univ Bergen, Bergen, Norway.
   Abdus Salaam Int Ctr Theoret Phys, Trieste, Italy.
   CNRS INSU, URA 1875, Ctr Europeen Rech & Format Avanceen Calcul Sci, Toulouse, France.
   NYU, New York, NY 10012 ,USA.
   Natl Oceanog Ctr Southampton, Southampton, Hants, England.
   Ctr Natl Rech Meteorol CNRM GAME, Toulouse, France.
   McGill Univ, Montreal, PQ, Canada.
   CNRS Ifremer IRD UBO, UMR 6523, Lab Phys Oceans, Plouzane, France.
   Japan Meteorol Agcy, Meteorol Res Inst, Tsukuba, Ibaraki 305, Japan.
   CSIRO, Ctr Australian Weather & Climate Res, Hobart, Tas, Australia.
C2 NOAA, USA
   UNIV ARIZONA, USA
   LLNL, USA
   NCAR, USA
   GEOMAR, GERMANY
   UNI RES BERGEN, NORWAY
   CSIRO, AUSTRALIA
   UNIV FLORIDA, USA
   INST A WEGENER, GERMANY
   UNIV TASMANIA, AUSTRALIA
   UNIV BERGEN, NORWAY
   ICTP, ITALY
   CERFACS, FRANCE
   UNIV NEW YORK NYU, USA
   NOC, UK
   CNRM, FRANCE
   UNIV MCGILL, CANADA
   CNRS, FRANCE
   JAPAN METEOROL AGCY, JAPAN
   CSIRO, AUSTRALIA
IF 2.927
TC 98
UR https://archimer.ifremer.fr/doc/00188/29904/28349.pdf
LA English
DT Article
DE ;Sea level;CORE global ocean-ice simulations;Steric sea level;Global sea level;Ocean heat content
AB 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.
PY 2014
PD JUL
SO Ocean Modelling
SN 1463-5003
PU Elsevier Sci Ltd
VL 78
UT 000336516100003
BP 35
EP 89
DI 10.1016/j.ocemod.2014.03.004
ID 29904
ER

EF