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  • Changement global ; Circulation océanique ; Effet de serre ; Eustatisme ; Holocène ; Interaction océan-atmosphère ; Littoral ; Modèle ; Niveau marin
  • Coastal environment ; Eustatism ; Global change ; Greenhouse effect ; Holocene ; Model ; Ocean atmosphere interaction ; Ocean circulation ; Sea level
  • The level of the ocean changes with time by a number of different causes. The rates and amplitudes of these changes differ. During the last 5000 years, the eustatic changes have been dominated by the redistribution of water masses due to changes
  • in the oceanic circulation systems. The sea-level changes to be expected in the next century are estimated on the basis of past and present sea-level changes and their driving forces; a possible future sea level rise in the next century will, at the most
  • 1996
  • Mediterranean coastal changes recorded in beach-rock cementation
  • 1996
  • In this paper, the geomorphological characteristics of the coasts of Turkey are described in general, and coastal changes and their effects on the coastal land use especially in the late Holocene have been stressed. Tuzla and Klaros have been used
  • as two examples of coastal change and geo-archaeological development on the Aegean coast.
  • 1996
  • This paper discusses certain criteria which have enabled the AA. to recognize marks left by rapid (coseismic) relative sea-level changes in coastal areas of the Eastern Mediterranean, in order to distinguish them from evidence of more gradual
  • relative sea-level changes.
  • 1996
  • Littoral zone and rapid climatic changes during the last 20,000 years. The Iberia study case
  • 1996
  • Late Holocene rapid coastal change in Western Anatolia-Büyük Menderes plain as a case study
  • 1996
  • Recent coastal changes in the Gulf of Valencia (Spain)
  • 1996
  • that have resulted from much longer-term changes in relative sea level.
  • 1996