|
|
|
|
|
Jasper Donker, Marcel Van Maarseveen and Gerben Ruessink
Coastal foredunes are highly dynamic landforms because of rapid erosion by waves and currents during storm surges in combination with gradual accretion by aeolian transport during more quiescent conditions. While our knowledge into the mechanisms behind ...
ver más
|
|
|
|
|
|
|
|
|
Duncan Tamsett, Jason McIlvenny and Andrew Watts
The backscatter response of a seabed to an incident sonar signal is dependent on the carrier wave frequency: i.e., the seabed is acoustically colourful. Colour is implemented in a prototype three-frequency sidescan sonar system deployed in the Pentland F...
ver más
|
|
|
|
|
|
|
|
|
Zhiguo He, Peng Hu, Liang Zhao, Gangfeng Wu and Thomas Pähtz
Breaching of earthen or sandy dams/dunes by overtopping flow and waves is a complicated process with strong, unsteady flow, high sediment transport, and rapid bed changes in which the interactions between flow and morphology should not be ignored. This s...
ver más
|
|
|
|
|
|
|
|
|
Oliver M. Lopez, Khan Z. Jadoon and Thomas M. Missimer
Planning for use of a dune field aquifer for managed aquifer recharge (MAR) requires that hydraulic properties need to be estimated over a large geographic area. Saturated hydraulic conductivity of dune sands is commonly estimated from grain size distrib...
ver más
|
|
|
|