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Energy Trapping near the Equator in a Numerical Ocean Model
Energy Trapping Equator Numerical Ocean Model
2009/2/16
The trapped equatorial standing modes described theoretically by Gent (1979) are reproduced in a single vertical-mode numerical ocean model. integrations are carried out in domains whose longitudinal ...
Long waves are affected by bottom topography and under certain conditions may be trapped along topographical contours which then act as wave guides transmitting wave energy for great distances with li...
Trapping of Waves by a Constant Slope internal Interface in a Two-Layer Ocean
Constant Slope perturbation equation Two-Layer Ocean
2009/2/7
It is well known that “edge” and “continental shelf” waves can be trapped by a constant slope nearshore bottom; in a two-layer ocean of great constant depth, a constant slope internal interface, as we...
Trapping of a Coastal Density Front by the Bottom Boundary Layer
Coastal Density Front Bottom Boundary Layer Trapping
2008/12/16
The dynamics of a surface-to-bottom density front on a uniformly sloping continental shelf and the role of density advection in the bottom boundary layer are examined using a three-dimensional, primit...
Coastal Trapping and Funneling Effects on Storm Surges in the Meghna Estuary in Relation to Cyclones Hitting Noakhali–Cox’s Bazar Coast of Bangladesh
Coastal Trapping Bangladesh Meghna Estuary Funneling Effects
2008/11/5
Studies are described that use a fine-resolution numerical model and incorporate the islands and detailed bottom topography of the Meghna estuary. They show that depending on the characteristics of th...