A numerical model for shoaling and refraction of third-order Stokes waves over an irregular bottom /

"May 1987."

Lower Green Bay hydrodynamic and mass transport : numerical model study /

"December 1987."

A user's guide to SHALWV, numerical model for simulation of shallow-water wave growth, propagation and decay.

"June 1987."

Numerical model investigation of Mississippi Sound and adjacent areas /

"February 1985."

A numerical model for predicting the effects of landslide-generated water waves /

Final report.

Savannah Harbor investigation and model study. numerical model study /

"September 1979."

Effects of proposed harbor modifications on wave conditions, harbor resonance, and tidal circulation at Fish Harbor, Los Angeles, California : Physical and numerical model investigations /

"June 1985."

Fisherman's Wharf area, San Francisco Bay, California, design for wave protection : physical and numerical model investigation /

Includes abstract.

Wave response of the proposed harbor at Agat, Guam : numerical model investigation /

"March 1987."

Salinity changes in Pontchartrain Basin Estuary resulting from Bonnet Carré freshwater diversion : numerical model investigation /

"February 1997."

MAC3D : numerical model for reservoir hydrodynamics with application to bubble diffusers /

"July 1998."

Lake Erie international jetport model feasibility investigation : report 17-4 : numerical model feasibility study /

"April 1977."

A Numerical model to evaluate proposed ground-water allocations in southwest Kansas /

Bibliography: p. 28, 30.

New numerical model of stimulated Brillouin scattering in optical fibres with nonuniformity

A new numerical model which incorporates Brillouin shift frequency variations arising from fibre inhomogeneities has been developed for stimulated Brillouin scattering in optical fibres. This enables simulations of backscattered and transmitted power as functions of input power based only on known physical and material parameters as well as the polarisation factor and the measured Brillouin gain linewidth for the fibre. Agreement between modelled and experimental power characteristics for a CW input is excellent.

Investigation of spatial patterns of ground-water exchange with lakes, using a three-dimensional numerical model

Hydrogeologic variables controlling groundwater exchange with inflow and flow-through lakes were simulated using a three-dimensional numerical model (MODFLOW) to investigate and quantify spatial patterns of lake bed seepage and hydraulic head distributions in the porous medium surrounding the lakes. Also, the total annual inflow and outflow were calculated as a percentage of lake volume for flow-through lake simulations. The general exponential decline of seepage rates with distance offshore was best demonstrated at lower anisotropy ratio (i.e., Kh/Kv = 1, 10), with increasing deviation from the exponential pattern as anisotropy was increased to 100 and 1000. 2-D vertical section models constructed for comparison with 3-D models showed that groundwater heads and seepages were higher in 3-D simulations. Addition of low conductivity lake sediments decreased seepage rates nearshore and increased seepage rates offshore in inflow lakes, and increased the area of groundwater inseepage on the beds of flow-through lakes. Introduction of heterogeneity into the medium decreased the water table and seepage ratesnearshore, and increased seepage rates offshore in inflow lakes. A laterally restricted aquifer located at the downgradient side of the flow-through lake increased the area of outseepage. Recharge rate, lake depth and lake bed slope had relatively little effect on the spatial patterns of seepage rates and groundwater exchange with lakes.