Finite element solution methods for circulation in estuaries
January 1, 1984
In this paper, the shallow water equations are used to approximate the depth-mean circulation in estuaries. The time scales of the motions can be conveniently divided into three ranges: 1) low-frequency (residual) variations with periods of two days or longer, 2) tidal-frequency variations, and 3) high-frequency variations with periods of an hour or shorter. The emphasis here will be on the tidal-period variations that are characterized by line spectra and thus allow a harmonic decomposition of the governing equations.
Citation Information
| Publication Year | 1984 |
|---|---|
| Title | Finite element solution methods for circulation in estuaries |
| Authors | Roy A. Walters |
| Publication Type | Book Chapter |
| Publication Subtype | Book Chapter |
| Index ID | 70174598 |
| Record Source | USGS Publications Warehouse |
| USGS Organization | San Francisco Bay-Delta; Pacific Regional Director's Office |