In order to quantify the effects of mutual feedbacks between geomorphology and benthic activity, we present a twoway coupled idealised sand wave model. This model allows for an extensive parameter analysis and gives insight in the effects of different time scales. Our analysis shows that the behaviour of the coupled system is essentially different from that of an abiotic system. Where in the latter, the basic state (flat bed) is essentially static, in the former, biomass may show growth (or decay). In turn, this affects hydro- and sediment dynamics, such that the basic state can be considered dynamic
Field observations in the Dover Strait (Le Bot and Trentesaux, 2004) show sandy bed patterns in an e...
International audienceAbstract Wave-dominated sandy beaches are highly valued by societies and are a...
International audiencePredicting the evolution of mound formations in the nearshore, both natural (e...
We use a linear stability approach to develop a process-based morphodynamic model including a two-wa...
The coastal environment shows a wide range of bed patterns, for which sandwaves and sandbanks are am...
The coastal environment shows a wide range of bed patterns, for which sandwaves and sandbanks are th...
Observations from the field show that the spatial distribution of benthic organisms is strongly corr...
Sand waves are rhythmic features on the bottom of shallow seas. Their shape drives the habitat selec...
Tidal sand waves are dynamic bedforms found in coastal shelf seas. Moreover, these areas are inhabit...
There is growing recognition of the importance of feedbacks between organisms and physical forces in...
Coastal morphodynamic and hydrodynamic processes impose a first-order control on biogeochemical cycl...
The bed of the North Sea is covered by sand waves and houses a great number of macrobenthic animals....
Changes in relative sea level, nutrient and sediment loading, and ecological characteristics expose ...
ABSTRACT: Changes in relative sea level, nutrient and sediment loading, and ecological characteristi...
Epi-benthic organisms play a strong role in controlling pelagic-benthic mass transfer rates by direc...
Field observations in the Dover Strait (Le Bot and Trentesaux, 2004) show sandy bed patterns in an e...
International audienceAbstract Wave-dominated sandy beaches are highly valued by societies and are a...
International audiencePredicting the evolution of mound formations in the nearshore, both natural (e...
We use a linear stability approach to develop a process-based morphodynamic model including a two-wa...
The coastal environment shows a wide range of bed patterns, for which sandwaves and sandbanks are am...
The coastal environment shows a wide range of bed patterns, for which sandwaves and sandbanks are th...
Observations from the field show that the spatial distribution of benthic organisms is strongly corr...
Sand waves are rhythmic features on the bottom of shallow seas. Their shape drives the habitat selec...
Tidal sand waves are dynamic bedforms found in coastal shelf seas. Moreover, these areas are inhabit...
There is growing recognition of the importance of feedbacks between organisms and physical forces in...
Coastal morphodynamic and hydrodynamic processes impose a first-order control on biogeochemical cycl...
The bed of the North Sea is covered by sand waves and houses a great number of macrobenthic animals....
Changes in relative sea level, nutrient and sediment loading, and ecological characteristics expose ...
ABSTRACT: Changes in relative sea level, nutrient and sediment loading, and ecological characteristi...
Epi-benthic organisms play a strong role in controlling pelagic-benthic mass transfer rates by direc...
Field observations in the Dover Strait (Le Bot and Trentesaux, 2004) show sandy bed patterns in an e...
International audienceAbstract Wave-dominated sandy beaches are highly valued by societies and are a...
International audiencePredicting the evolution of mound formations in the nearshore, both natural (e...