Computing extreme meteorologically induced currents, with application to the northwest European continental shelf

Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model

“…As a result, some of small-scale disturbances generated inside the CM domain could be trapped near the CM open boundary if the large-scale PM model results are used directly to specify the CM boundary values. The present two-way nesting technique also uses the barotropic boundary condition suggested by Davies and Flather (1978) for the external mode, and the adaptive radiation condition modified from the scheme suggested by Orlanski (1976) for the internal mode at the CM open boundary to allow small-scale disturbances to propagate outward through the CM open boundary as freely as possible.…”

Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model

“…As a result, some of small-scale disturbances generated inside the CM domain could be trapped near the CM open boundary if the large-scale PM model results are used directly to specify the CM boundary values. The present two-way nesting technique also uses the barotropic boundary condition suggested by Davies and Flather (1978) for the external mode, and the adaptive radiation condition modified from the scheme suggested by Orlanski (1976) for the internal mode at the CM open boundary to allow small-scale disturbances to propagate outward through the CM open boundary as freely as possible.…”

A First Attempt to Describe the Real-Time Behavior and Fate of Marine Litter Items in the Nearshore and Foreshore under Low Energetic Marine Conditions

“…The wind stress produces variations in the current velocity with depth. According to the "law of wall" [35,36]:…”

Modelling the non‐linear interaction of wind and tide: Its influence on current profiles

“…Thus the u and v-components of velocity are expanded as where $: and $; are additional functions specifically chosen to improve convergence in the near-surface layer, f,(a) are chosen as eigenfunctions of the eddy viscosity profile,15s17 a = z / h is the normalized vertical co-ordinate, with h the water depth, and A#) and Br(t) are coefficients to be determined using the Galerkin method. Having computed these coefficients, the current at any depth can be readily determined from expansion (8). The additional functions ('enhancement' functions) $: and $2 were taken as the trigonometric functions used in Reference 15.…”

Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model

“…As a result, some of small-scale disturbances generated inside the CM domain could be trapped near the CM open boundary if the large-scale PM model results are used directly to specify the CM boundary values. The present two-way nesting technique also uses the barotropic boundary condition suggested by Davies and Flather (1978) for the external mode, and the adaptive radiation condition modified from the scheme suggested by Orlanski (1976) for the internal mode at the CM open boundary to allow small-scale disturbances to propagate outward through the CM open boundary as freely as possible.…”

A First Attempt to Describe the Real-Time Behavior and Fate of Marine Litter Items in the Nearshore and Foreshore under Low Energetic Marine Conditions

“…The wind stress produces variations in the current velocity with depth. According to the "law of wall" [35,36]:…”

Modelling the non‐linear interaction of wind and tide: Its influence on current profiles

“…Thus the u and v-components of velocity are expanded as where $: and $; are additional functions specifically chosen to improve convergence in the near-surface layer, f,(a) are chosen as eigenfunctions of the eddy viscosity profile,15s17 a = z / h is the normalized vertical co-ordinate, with h the water depth, and A#) and Br(t) are coefficients to be determined using the Galerkin method. Having computed these coefficients, the current at any depth can be readily determined from expansion (8). The additional functions ('enhancement' functions) $: and $2 were taken as the trigonometric functions used in Reference 15.…”

Far-field effects of tidal energy extraction in the Minas Passage on tidal circulation in the Bay of Fundy and Gulf of Maine using a nested-grid coastal circulation model

“…As a result, some of small-scale disturbances generated inside the CM domain could be trapped near the CM open boundary if the large-scale PM model results are used directly to specify the CM boundary values. The present two-way nesting technique also uses the barotropic boundary condition suggested by Davies and Flather (1978) for the external mode, and the adaptive radiation condition modified from the scheme suggested by Orlanski (1976) for the internal mode at the CM open boundary to allow small-scale disturbances to propagate outward through the CM open boundary as freely as possible.…”

A First Attempt to Describe the Real-Time Behavior and Fate of Marine Litter Items in the Nearshore and Foreshore under Low Energetic Marine Conditions

“…The wind stress produces variations in the current velocity with depth. According to the "law of wall" [35,36]:…”

Modelling the non‐linear interaction of wind and tide: Its influence on current profiles

“…Thus the u and v-components of velocity are expanded as where $: and $; are additional functions specifically chosen to improve convergence in the near-surface layer, f,(a) are chosen as eigenfunctions of the eddy viscosity profile,15s17 a = z / h is the normalized vertical co-ordinate, with h the water depth, and A#) and Br(t) are coefficients to be determined using the Galerkin method. Having computed these coefficients, the current at any depth can be readily determined from expansion (8). The additional functions ('enhancement' functions) $: and $2 were taken as the trigonometric functions used in Reference 15.…”