Dune dynamics and associated sedimentary fluxes have been estimated over a period of a week in the river Seine characterised by limited sediment supply. Distributed into two corridors, typical medium and small dunes associated with fluvial environments have been characterised from multibeam data acquired on four dates, 23-29 March 2021, after a limited peak flood. Dune morphometric parameters have been quantified on cross-dune 1 m spacing of bed elevation profiles and dune migration rates have been calculated by analysing successive multibeam acquisitions. Evidence of limited sediment supply conditions have been recognised from areas uncovered by mobile sediment in the troughs between medium dunes. Under such conditions, bedload transport a...
International audienceThree methods used to estimate river bedload discharges were compared in a lar...
Dunes are common bed forms in sand bed rivers and are of central interest in water management purpos...
International audienceMarine sand dunes and sand banks can exhibit rapid morphological changes in co...
Dune formation in river systems influences sediment transport, flow characteristics, bank erosion, f...
As dunes move along the riverbed, they change in size, shape, and arrangement. This involves sedimen...
Delta areas around the world are densely populated, and feature an incredible amount of economic act...
Dunes are the most common bed forms in lowland river channels consisting of sand and gravel, generat...
In natural rivers, flow discharge may fluctuate across a range of time scales – from diurnal to seas...
Dunes are the most common bedforms present in nearly all fluvial channels. Because of their dimensio...
Dunes are bedforms commonly found in sand-bedded rivers. They are important sources of flow resistan...
Sandy river beds are dominated by rhythmic features known as dunes. Experimental investigations of t...
(IF 3.62; Q1)International audienceUnderstanding the response of the intertidal dunes to the varying...
International audienceSandy river beds are dominated by rhythmic features known as dunes. Experiment...
The dunes that cover the beds of most alluvial channels change in size and shape over time and in sp...
International audienceThree methods used to estimate river bedload discharges were compared in a lar...
Dunes are common bed forms in sand bed rivers and are of central interest in water management purpos...
International audienceMarine sand dunes and sand banks can exhibit rapid morphological changes in co...
Dune formation in river systems influences sediment transport, flow characteristics, bank erosion, f...
As dunes move along the riverbed, they change in size, shape, and arrangement. This involves sedimen...
Delta areas around the world are densely populated, and feature an incredible amount of economic act...
Dunes are the most common bed forms in lowland river channels consisting of sand and gravel, generat...
In natural rivers, flow discharge may fluctuate across a range of time scales – from diurnal to seas...
Dunes are the most common bedforms present in nearly all fluvial channels. Because of their dimensio...
Dunes are bedforms commonly found in sand-bedded rivers. They are important sources of flow resistan...
Sandy river beds are dominated by rhythmic features known as dunes. Experimental investigations of t...
(IF 3.62; Q1)International audienceUnderstanding the response of the intertidal dunes to the varying...
International audienceSandy river beds are dominated by rhythmic features known as dunes. Experiment...
The dunes that cover the beds of most alluvial channels change in size and shape over time and in sp...
International audienceThree methods used to estimate river bedload discharges were compared in a lar...
Dunes are common bed forms in sand bed rivers and are of central interest in water management purpos...
International audienceMarine sand dunes and sand banks can exhibit rapid morphological changes in co...