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  • Three-dimensional topographic on the foreshore zone of sandy beaches
  • Cordon littoral ; Erosion marine ; Granulométrie ; Géographie de l'Asie ; Honshu ; Ibaraki préfecture ; Japon ; Littoral ; Modèle ; Niveau marin ; Sable ; Topographie
  • -dimensional beach model in the foreshore zone on sandy beaches was constructed. - (SGA)
  • Topographic surveys are carried out to elucidate the characteristics of topographic changes in the foreshore zone of two study sites on the Kashima Coast, Ibaraki Prefecture (Kanto). Three types of topographic change were put in order and a three
  • The Antarctic ice sheet during the last glacial interglacial cycle : a three-dimensional experiment
  • Antarctique ; Expérimentation ; Glace ; Glaciaire ; Géographie des régions polaires ; Modèle ; Paléoclimatologie
  • Un modèle thermo-mécanique complètement tri-dimensionnel pour la couche de glace de l'Antarctique entier est employé pour simuler la réaction de la couche de glace durant le dernier cycle glaciaire-interglaciaire, en ce qui concerne les conditions
  • Three-dimensional structure of flow at a confluence of river channels with discordant beds
  • Canada ; Capacité de charge ; Confluence ; Cours d'eau ; Ecoulement ; Modèle ; Québec ; Transport sédimentaire ; Turbulence ; Variation spatiale
  • Canada ; Carrying capacity ; Confluent ; Model ; Quebec ; Runoff ; Sediment transport ; Spatial variation ; Stream ; Turbulence
  • This paper presents data on the detailed structure of three-dimensional mean and turbulent flow for different hydraulic conditions at the confluence of natural rivers with discordant beds. The objectives of the paper are : 1) to describe the three
  • -dimensional field of flow at a junction of natural channels; 2) to assess the role of changes in bed morphology that occur during transport-effective events on the structure of flow at a confluence; and 3) to examine how the structure of three-dimensional flow
  • Three-dimensional groundwater flow system in the Imaichi alluvial fan, Tochigi Prefecture, Japan
  • Cône de déjection ; Deutérium ; Eau souterraine ; Honshū ; Hydrochimie ; Irrigation ; Japon ; Modèle ; Nappe aquifère ; Oxygène 18 ; Qualité de l'eau ; Recharge naturelle ; Saison ; Utilisation du sol
  • Alluvial cone ; Aquifer ; Deuterium ; Groundwater ; Honshu ; Hydrochemistry ; Irrigation ; Japan ; Land use ; Model ; Natural recharge ; Oxygen 18 ; Season ; Water quality
  • The objective of this study is to make clear the three-dimensional structure of groudwater flow system and the mixing of recharged waters in the aquifer of the Imaichi alluvial fan wich has a complex geological structure, topography, and land use
  • An introduction to three-dimensional climate modelling.
  • Atmosphère ; Climat ; Climat mondial ; Climatologie ; Glace ; Géographie physique ; Modèle ; Modèle numérique ; Modèle tri-dimensionnel ; Océan ; Simulation ; Variation climatique
  • A three-dimensional analysis on lift-off velocities of sand grains in wind-blown sand flux
  • Chine ; Eolien ; Etude comparée ; Gansu ; Modèle ; Sable ; Transport éolien ; Vent
  • Aeolian features ; Aeolian transport ; China ; Comparative study ; Gansu ; Model ; Sand ; Wind
  • This paper focuses on a key problem in wind-blown sand transport research, the lift-off velocities of sand grains. A three-dimensional grain-bed collision model comprising an impact sand grain, a creeping sand grain and a sustaining grain
  • and ejected velocities gained by the three-dimensional model are lower than the corresponding ones done by two-dimensional model apart from the horizontal rebound velocity. It also shows the lateral velocity and the lateral angular velocity, as well
  • is presented. Based on this model, the analytical formulae of sand grains'linear and angular velocities are derived. Comparisons of the results with the results gained by a two-dimensional grain-bed collision model show that all components of both rebound
  • as the upward angular velocity, cannot be obtained by a two-dimensional model, and cannot be ignored when the impact velocity is high.
  • Simulated slope development sequences in a three-dimensional context
  • Downvalley sequences of slope profiles have been inferred to represent temporal sequences. Results from a simulation model are presented which demonstrate that for a slope system in dynamic equilibrium, the downvalley variation in form is best
  • Prediction of the shape of a shallow failure on a mountain slope: the three-dimensional multi-planar sliding surface method
  • Japon ; Modèle ; Montagne ; Mouvement de masse ; Précipitation ; Prévision ; Ruissellement ; Versant
  • Forecast ; Japan ; Mass movement ; Model ; Mountain ; Precipitation ; Rill wash ; Slope
  • A three-dimensional multi-planar sliding surface method developed from the two-dimensional method is proposed to identify the shape and/or volume of a shallow failure that appears on a mountain slope during heavy rainfall. It was applied
  • to a digital elevation model to determine the site and form of a critical sliding mass on a mountain slope. The method was applied to an actual mountain slope on which a shallow failure caused by heavy rainfall took place. The most probable unstable mass
  • calculated by the model was almost the same as that at the failed site.
  • The application of computational fluid dynamics to natural river channels : three-dimensional versus two-dimensional approaches
  • Capacité de charge ; Confluence ; Cours d'eau ; Ecoulement fluvial ; Hydrodynamique ; Modèle ; Modèle numérique ; Rugosité ; Turbulence
  • Carrying capacity ; Confluent ; Hydrodynamics ; Model ; Numerical model ; Roughness ; Stream ; Stream flow ; Turbulence
  • models improve predictive ability and prediction utility compared to 2D applications. This is achieved through comparing the predictions of both 3D and 2D models with high-quality field data. Identical boundary conditions, obtained from a confluence
  • within a gravel-bed river system with high relative roughness, are defined for each model.
  • Transferable parameterization methods for distributed hydrological and agroecological catchment models
  • Agrosystème ; Allemagne de l'Ouest ; Bassin-versant ; Géographie physique ; Humidité du sol ; Informatique ; Modèle numérique ; Méthodologie ; Prévision ; Réseau de drainage ; Sol ; Sédiment
  • The application of distributed hydrological and agroecological models requires the knowledge of model parameters, boundary conditions and initial conditions for each element of the three-dimensional finite difference grid in the catchment area under
  • survey. This paper discusses methods suitable for processing the values of such parameters. The Digital Relief Model can be used to compute the ecologically relevant morphographic parameters, the three dimensional Digital Sediment and Soil Model
  • Three-dimensional flow modelling and sediment transport in the River Klarälven
  • Charge solide ; Confluence ; Cours d'eau ; Ecoulement ; Ecoulement fluvial ; Ecoulement secondaire ; Géométrie hydraulique ; Modèle ; Rugosité ; Sable ; Suède ; Transport sédimentaire
  • Channel geometry ; Confluent ; Model ; Roughness ; Runoff ; Sand ; Sediment load ; Sediment transport ; Stream ; Stream flow ; Sweden
  • A three-dimensional flow model that uses the RNG turbulence model and a non-equilibrium wall function was applied to the River Klarälven in the southwest part of Sweden. The objectives were to study the nature of the flow in the river bifurcation
  • and to investigate the short-term sediment transport patterns in the river. The numerical models were built and verified using extensive field data. Based on model outputs, observations are made about the velocity vectors and the secondary flow patterns. The main
  • Numerical computations of a theoretical model of ribbed moraine formation
  • Drainage sous-glaciaire ; Drumlin ; Glaciaire ; Irlande ; Modèle ; Modèle numérique ; Moraine
  • Drumlin ; Glacial features ; Ireland ; Model ; Moraine ; Numerical model ; Subglacial drainage
  • as ribbed moraine. However, these investigations have left unanswered the question of whether the theory is capable of producing fully three-dimensional bedforms such as drumlins. The AA. show that, while the three-dimensional calculations show realistic
  • quasi-three-dimensional features such as dislocations in the ribbing pattern, they do not produce genuine three-dimensional drumlins. The AA. suggest that this inadequacy is due to the treatment of subglacial drainage in the theory as a passive variable
  • , and thus that the three-dimensional forms may be associated with conditions of sufficient subglacial water flux.
  • The AA. develop numerical solutions of a theoretical model which has been proposed to explain the formation of subglacial bedforms. The model has been shown to have the capability of producing bedforms in two dimensions, when they may be interpreted
  • Karst landform development in a three-dimensional theoretical model
  • Chine ; Dissolution karstique ; Doline ; Guizhou ; Infiltration ; Karst ; Karstification ; Modèle ; North Island ; Nouvelle-Zélande ; Ruissellement ; Tectonique ; Topographie
  • Carbonate dissolution ; China ; Doline ; Guizhou ; Infiltration ; Karst ; Karstification ; Model ; New Zealand ; North Island ; Rill wash ; Tectonics ; Topography
  • A three-dimensional process-response model is developed that assesses the minimum requirements for karst landform evolution, the effect of different starting conditions on end-stage landforms, and whether different landform types are the results
  • of different environments or merely represent successive stages under unchanging conditions. Results of 7 different runs of the model are presented as block diagrams, each run representing a different set of conditions. Variables tested that influence the rate
  • Three-dimensional hydrogeological modelling application to the Alverà mudslide (Cortina d'Ampezzo, Italy)
  • Alpes ; Glissement de terrain ; Hydrogéologie ; Infiltration ; Italie ; Modèle ; Montagne ; Nappe phréatique ; Précipitation ; Système d'information géographique
  • Alps (The) ; Geographical information system ; Hydrogeology ; Infiltration ; Italy ; Landslide ; Model ; Mountain ; Phreatic ground water ; Precipitation
  • Within the framework of Geographic Information System (GIS), the distributed three-dimensional groundwater model MODFLOW is applied to evaluate the groundwater processes of the hydrogeological system in the Alverà landslide. The application
  • of this model has permitted an analysis of the spatial distribution of the structure (DTM and landslide bottom) and the mass transfer elements of the hydrogeological system. The field survey suggested zoning the area on the basis of the recharge, groundwater
  • A coupling three dimensional baroclinic model of Biwa Lake air-water system
  • Biwa ; Circulation de l'eau ; Cyclone ; Dynamique de l'atmosphère ; Honshū ; Hydrodynamique ; Japon ; Lac ; Modèle numérique ; Température de l'eau ; Variation saisonnière ; Vent
  • Atmospheric dynamics ; Cyclone ; Honshu ; Hydrodynamics ; Japan ; Lake ; Numerical model ; Seasonal variation ; Water circulation ; Water temperature ; Wind
  • A numerical model coupling atmosphere with hydrodynamics is set up in this paper, and is applied in the experimental study of Lake Biwa. Discussion of the results.
  • Modelling three-dimensional flow structures and patterns of boundary shear stress in a natural pool-riffle sequence
  • Cours d'eau ; Ecoulement fluvial ; England ; Géométrie hydraulique ; Hampshire ; Modèle ; Profil longitudinal ; Royaume-Uni ; Simulation ; Transport sédimentaire
  • Channel geometry ; England ; Hampshire ; Longitudinal section ; Model ; Sediment transport ; Simulation ; Stream ; Stream flow ; United Kingdom
  • Three-dimensional flow structure around small-scale bedforms in a simulated gravel-bed environment
  • Cours d'eau ; Ecoulement ; Ecoulement fluvial ; Gravier ; Lit fluvial ; Modèle ; Simulation ; Turbulence
  • Gravel ; Model ; River bed ; Runoff ; Simulation ; Stream ; Stream flow ; Turbulence
  • This paper presents high-resolution three-dimensional data illustrating the effects of pebble clusters on turbulent flow characteristics in a simulated gravel-bed environment. Past research has tended to focus on only 2 flow components : downstream
  • ) model and will elucidate more explicitely bed-flow interactions in gravel-bed environments.
  • Three-dimensional secondary surface geomorphology of submarine landslides on northwest Pacific plate guyots
  • Bathymétrie ; Guyot ; Géophysique ; Marge continentale ; Modèle ; Mouvement de masse ; Pacifique ; Pacifique Nord-Ouest ; Séisme ; Tectonique de plaques ; Tectonique globale
  • Bathymetry ; Continental margin ; Earthquake ; Geophysics ; Global tectonics ; Mass movement ; Model ; North-West Pacific Ocean ; Pacific Ocean;Pacific Region ; Plate tectonics ; Seamount
  • Influence of experimental removal of large woody debris on spatial patterns of three-dimensional flow in a meander bend
  • Cours d'eau ; Débris ligneux ; Ecoulement fluvial ; Etats-Unis ; Expérimentation ; Géométrie hydraulique ; Midwest ; Modèle ; Méandre
  • Channel geometry ; Experimentation ; Meander ; Midwest ; Model ; Stream ; Stream flow ; United States of America
  • Three-dimensional numerical model simulations of airflow over mountainous terrain: a comparison with observations
  • Ascendance ; Climatologie ; Direction ; Dynamique de l'atmosphère ; Déviation du vent ; Effet de foehn ; Effet orographique ; Etats-Unis ; Géographie physique ; Humidité atmosphérique ; Hydrodynamique de l'atmosphère ; Ligne de flux ; Modèle
  • ; Modèle numérique ; Montagne ; Mouvement orographique ; Nuage ; Nuage orographique ; Onde de relief ; Rocky Mountains ; Simulation ; Température ; Thermodynamique ; Topographie ; Turbulence ; Vent ; Vitesse
  • Essai de mise au point d'un modèle numérique tri-dimensionnel pour la simulation de l'effet hydrodynamique d'obstacle. Deux cas sont distingués suivant le contexte thermique. Les résultats sont en accord assez satisfaisant avec les perturbations