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  • Sea level
  • Bog ; Coastal dynamics ; Coastal environment ; Foraminifera ; Global change ; Indicator ; Quaternary ; Sea level
  • Changement global ; Dynamique littorale ; Foraminifère ; Indicateur ; Littoral ; Marais ; Niveau marin ; Quaternaire
  • This report examines recent developments in relation to present (and anticipated future) sea level, Quaternary sea-level fluctuations, the response of coastal landforms to sea-level change and the use of biological indicators of sea-level change.
  • Sea level
  • Bibliography ; Coastal environment ; Eustatism ; Global change ; Greenhouse effect ; Impact ; Quaternary ; Sea level ; Shoreline
  • Bibliographie ; Changement global ; Effet de serre ; Eustatisme ; Impact ; Ligne de rivage ; Littoral ; Niveau marin ; Quaternaire
  • This report will concentrate on aspects of Quaternary sea-level change, summaries of trends in sea-level over recent decades from tide gauges, and predictions of future sea-level change and the anticipated responses of the coast.
  • Climatic change, ice sheets and sea level in Sea level ice and climatic change.
  • Changements du géoïde ; Concept ; Dynamique océanique ; Eustatisme ; Généralités sur la géographie ; Monde ; Mouvements verticaux ; Niveau marin ; Océan ; Océan mondial ; PICG 200
  • Eustasy can no longer be defined as world wide simultaneous changes in sea level, but must be redefined as ocean level changes or any absolute sea level changes regardless of causation and including both the vertical and horizontal changes
  • of the geoid surface as well as changes of the dynamic sea surface topography. In the field, only relative sea level changes can be observed (Author).
  • Possible effects of recent changes in sea level on the biota of a Caribbean reef flat and predicted effects of rising sea levels in Proceedings. Volume 3. Symposia and seminars.
  • Prediction of the changes in biota that would result on a semi-intertidal reef flat of Panama from a slight rise in sea level.
  • Holocene sea-level changes and coastal processes on the south coast of Ireland: corals and the problems of sea-level methodology in temperate waters in Proceedings. Volume 3. Symposia and seminars.
  • A discussion on indicators of coastline and sea-level changes in Ireland.
  • Sea level rise
  • Forecast ; Global change ; Greenhouse effect ; New Zealand ; Sea level
  • Changement global ; Effet de serre ; Niveau marin ; Nouvelle-Zélande ; Prévision
  • This paper concerns a few of many important aspects of the treatment given to sea-level rise postulated to attend global warming under the greenhouse warming group of hypotheses. Particular atteention is paid to the last 5 years of this debate.
  • Should Quaternary sea-level changes be used to correct glacier ELAs, vegetation belt altitudes and sea level temperatures for inferring climate changes ?
  • Altitudinal zonation ; Climatic change ; Glacier ; Quaternary ; Sea level ; Snow line ; Vegetation
  • Changement climatique ; Glacier ; Limite d'enneigement ; Niveau marin ; Quaternaire ; Végétation ; Zonation altitudinale
  • Changes in the altitudes of glacier snowlines (ELAs) and the altitudes of montane vegetation belts (VBAs) measure Quaternary climatic change. Here, the A. shows that a recently proposed correction for these and other similar approaches is faulty
  • Sea level is not level : the case for a new approach to predicting UK sea-level rise
  • Climatic change ; Coastal environment ; Forecast ; Geophysics ; Global change ; Methodology ; Model ; Sea level ; United Kingdom
  • Changement climatique ; Changement global ; Géophysique ; Littoral ; Modèle ; Méthodologie ; Niveau marin ; Prévision ; Royaume-Uni
  • The AA. argue that the global (Intergovernmental Panel on Climate Change) IPCC sea-level values should be replaced by a suite of regional values, to take into account known processes that cause regional changes in sea-surface topography
  • . Quantification of these processes, which include gravitational adjustments of the ocean surface and nearshore ocean-density changes, requires the use of numerical ocean and geophysical models. These 2 additional mechanisms are not included in IPCC assessments
  • . A combined modelling/geological approach will produce more robust regional sea-level predictions for the UK.
  • Sea level
  • Climatic warming ; Coastal dynamics ; Earthquake ; Eustatism ; Glacio eustatic change ; Global change ; Ice sheet ; Model ; Quaternary ; Sea level ; Tsunami
  • Calotte glaciaire ; Changement global ; Dynamique littorale ; Eustatisme ; Glacio-eustatisme ; Modèle ; Niveau marin ; Quaternaire ; Réchauffement climatique ; Séisme ; Tsunami
  • change over the Late Quaternary, and the success or otherwise in trying to monitor ongoing global sea-level change.
  • This report cannot attempt to review all that has been written on sea level in the last one or two years. Instead, it examines the extent to which it has been possible to reconstruct or explain the past pattern of truly global (eustatic) sea-level
  • Symposium. Holocene sea-level changes.
  • Flytting og endring i levekar Migrations and changes in levels of living
  • Sea levels : change and variability during warm intervals
  • Climate ; Climatic change ; Climatic warming ; Holocene ; Impact ; Interglacial ; Meltwater ; Sea level
  • Changement climatique ; Climat ; Eau de fonte ; Holocène ; Impact ; Interglaciaire ; Niveau marin ; Réchauffement climatique
  • Niveaux marins élevés : niveaux marins interglaciaires, changements du niveau terrestre. Changements de la glace et des océans : impulsions d'eau de fonte, élévation du niveau marin de l'Holocène moyen au supérieur, changements instrumentaux.
  • Sea level change: environmental and socio-economic impacts
  • Economic impact ; Fishery;Fishing ; Global change ; Impact study ; Ocean ; Sea level
  • Changement global ; Etude d'impact ; Impact économique ; Niveau marin ; Océan ; Pêche
  • Recent calculations that a rapid sea level rise is imminent, has prompted concerned efforts at meeting the socio-economic impacts that are likely to occur. These impacts, rather than being localized and temporary as has been true in the recent past
  • Analytical predictions of beach profile change in response to a sea-level rise in Geomorphology of changing coastlines.
  • Recent studies predict a sea-level rise of the order of 0.5 to 3.5 m by the year 2100. Beach profile translation and coastal erosion will, in most cases, accompany the rising level of the sea. Calculations for estimating potential erosion on a sandy
  • Sea levels : resolution and uncertainty
  • Biostratigraphy ; Diatom ; Foraminifera ; Forecast ; Geochemistry ; Holocene ; Pollen ; Remote sensing ; Satellite ; Sea level
  • This report briefly reviews the IPCC Fourth Assessment Report (AR4) sea-level summary and projections for future change. It then considers the development of high-resolution records of relative sea-level (RSL) change which have the potential
  • Sea level
  • Coastal erosion ; Coastal management ; Environmental management ; Global change ; Impact ; Model ; Sea level
  • Aménagement du littoral ; Changement global ; Erosion littorale ; Gestion de l'environnement ; Impact ; Modèle ; Niveau marin
  • This report focuses on assessments of the impact of sea-level rise on contemporary geomorphic systems (sea-level projections, coastal system response) and some of the socioeconomic aspects of these impacts.
  • Late Holocene sea-level change on Rota and Guam, Mariana Islands, and its constraint on geophysical predictions
  • C 14 dating ; Geophysics ; Holocene ; Micronesia ; Model ; Quaternary ; Reef ; Sea level ; Vertical movement
  • Holocene emergent reefs and notches are well distributed on Rota and Guam. Relative sea-level changes at these islands are reconstructed based on geomorphological observations and borings on present and emergent reefs, together with 54 radiocarbon
  • dates. Reconstructed late Holocene sea-level change in the Mariana Islands provides constraints on geophysical models of sea-level variations.
  • Late Holocene sea-level changes seen from prehistoric settlements
  • Radiocarbon dates from prehistoric human settlements in Varanger, Finnmark, North Norway, are used to examine Holocene relative sea-level changes. (JH).
  • Sea level variability
  • Coastal environment ; Eustatism ; Global change ; Greenhouse effect ; Holocene ; Model ; Ocean atmosphere interaction ; Ocean circulation ; Sea level
  • Changement global ; Circulation océanique ; Effet de serre ; Eustatisme ; Holocène ; Interaction océan-atmosphère ; Littoral ; Modèle ; Niveau marin
  • 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