Flow and transport in the Suwannee River estuary, Florida, 1999-2000: Analysis of data and three-dimensional simulations

2006 ◽  
Author(s):  
Jerad D. Bales ◽  
S.A. Tomlinson ◽  
Gina Tillis
1991 ◽  
Vol 24 (6) ◽  
pp. 171-177 ◽  
Author(s):  
Zeng Fantang ◽  
Xu Zhencheng ◽  
Chen Xiancheng

A real-time mathematical model for three-dimensional tidal flow and water quality is presented in this paper. A control-volume-based difference method and a “power interpolation distribution” advocated by Patankar (1984) have been employed, and a concept of “separating the top-layer water” has been developed to solve the movable boundary problem. The model is unconditionally stable and convergent. Practical application of the model is illustrated by an example for the Pearl River Estuary.


2011 ◽  
Vol 733 (1) ◽  
pp. 17 ◽  
Author(s):  
Kazunari Iwasaki ◽  
Shu-ichiro Inutsuka ◽  
Toru Tsuribe

1995 ◽  
Vol 100 (A12) ◽  
pp. 23779 ◽  
Author(s):  
Zi-Ping Sun ◽  
R. P. Turco ◽  
R. L. Walterscheid ◽  
S. V. Venkateswaran ◽  
P. W. Jones

2003 ◽  
Vol 478 ◽  
pp. 1-10 ◽  
Author(s):  
KRISTIAN B. DYSTHE ◽  
KARSTEN TRULSEN ◽  
HARALD E. KROGSTAD ◽  
HERVÉ SOCQUET-JUGLARD

Numerical simulations of the evolution of gravity wave spectra of fairly narrow bandwidth have been performed both for two and three dimensions. Simulations using the nonlinear Schrödinger (NLS) equation approximately verify the stability criteria of Alber (1978) in the two-dimensional but not in the three-dimensional case. Using a modified NLS equation (Trulsen et al. 2000) the spectra ‘relax’ towards a quasi-stationary state on a timescale (ε2ω0)−1. In this state the low-frequency face is steepened and the spectral peak is downshifted. The three-dimensional simulations show a power-law behaviour ω−4 on the high-frequency side of the (angularly integrated) spectrum.


Sign in / Sign up

Export Citation Format

Share Document