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- (1) Tracer waiting times and the steady-state evolution of a granular bed
- (10) The Development and Changes of Coastal Landscape Morphology of the Ganges-Brahmaputra-Meghna Mega Delta in Bangladesh
- (11) Response of deltas to differential water depths in the transverse direction: Tank experiments with bimodal grain-size sediment
- (12) Effects of vegetation on delta morphodynamics and sediment transport
- (13) Experiments of the formation of tidal channels
- (14) A new principle on morphodynamic stability and its application to shallow sea reclamation project
- (15) Autogenic submarine terrace formed by wave erosion during early stage of sea-level rise: implication from numerical experiments
- (16) Coevolution of minibasin subsidence and sedimentation: Experiments
- (17) Dynamics of the turbidity current generated by the 2011 Tohoku-Oki earthquake and tsunami
- (18) Submarine landslides and tsunamis
- (19) Interaction of granular flows and their boundaries: basal forces, particle kinematics, and bed erosion measured in a large vertically rotating drum flume
- (2) Armor Development from Decapitated Flash Flood Bores in Supply-Limited Flume Experiments
- (20) An improved sample preparation method for imaging microstructures of fine-grained marine sediment using microfocus X-ray CT and SEM
- (21) Analysis of grain fabric in turbidite sandstone using electron backscatter diffraction in the SEM
- (22) Measuring laboratory stratigraphy through image analysis
- (23) Advances in simulating fluvial sediment transport at basin-scale
- (24) Simulation of long-term erosion-sedimentation process using particle method
- (25) Morphodynamics of dunes under unidirectional wind
- (26)THE FORMATION OF BOUNDARY WAVES ON THE ICE SURFACE BY TURBULENT FLOW
- (27) Bedforms under polydirectional flow: a preliminary experiment using pure oscillatory flow
- (28) Migration rate of combined-flow bedform: an analogue experiment
- (29) 2D numerical simulation on migration and accumulation of snow bedforms
- (3) EXPERIMENTAL STUDY OF CONNECTIVITY IN MEANDERING RIVERS: IMPLICATIONS FOR STRATIGRAPHIC STRUCTURE OF BURIED CHANNELS
- (30) Experimental study of bedforms formed by supercritical density currents
- (4) Oblique shoreline progradation during the Quaternary regressive stage: case study from Yufutsu Plain, Hokkaido, Northern Japan
- (4) Theoretical Aspects of the Formation of River Bedforms
- (5) Holocene Beach landform and sedimentary structure affected by glacial-isostatic rebound in East Antarctic
- (6)Structure and development of the Holocene sandy gravel spit in the Osaka Plain
- (7) SEA LEVEL AND SEDIMENT SUPPLY FLUCTUATIONS DURING THE BOLLING-ALLEROD TO YOUNGER DRYAS TRANSITION REVEALED BY A 2D NUMERICAL MODELING OF THE CENTRAL ADRIATIC TRANSGRESSIVE RECORD
- (8) Depositional facies containing vertebrate fossils in the Upper Cretaceous Himenoura Group on the Koshikijima Islands, Kagoshima, Kyushu, Japan
- (9) Determining Fluvial Flow Conditions from Bed Set Geometry
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