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Journal ArticleDOI

An energy-conserving difference scheme for the storm surge equations1

Anita Sielecki
- 01 Mar 1968 - 
- Vol. 96, Iss: 3, pp 150-156
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TLDR
In this paper, a system of finite difference equations for storm surge prediction using forward time differences was constructed, and the scheme was tested for special simple geometrical configurations, and it was found to be stable without introducing smoothing operators.
Abstract
A system of finite difference equations for storm surge prediction has been constructed, using forward time differences. The scheme was tested for special simple geometrical configurations, and it was found to be stable without introducing smoothing operators. The variation with time of the total energy was, in each case, the test of stability. The small-scale oscillation of the energy with time (characteristic of forward difference schemes) was studied in detail. A method of reducing this effect is suggested. A completely implicit finite difference scheme is discussed from the point of view of stability and convergence. It is shown how the requirement of a convergent iterative process actually introduces a severe restriction on the ratio Δt/Δs, thus canceling the advantages of the otherwise unconditionally stable implicit schemes.

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A two-dimensional numerical sea model

TL;DR: In this paper, the authors developed a model for the detailed investigation of various types of North Sea storm surge, particularly the external surge, using a finite-difference grid and a step-by-step procedure in time.
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Northward flow in the Bering and Chukchi seas

TL;DR: In this article, the authors investigated the Bering and Chukchi sea shelves using a barotropic numerical model and found that in the presence of the winter seasonal wind stress from the northeast, observed northward transport through Bering Strait of 0.6 Sv for the 8-month winter season 1981-1982 can be driven by a sea level difference between the Pacific and Arctic oceans.
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A coupled ice‐ocean model of upwelling in the marginal ice zone

TL;DR: In this article, a dynamical coupled ice-ocean numerical model for the marginal ice zone (MIZ) is suggested and used to study upwelling dynamics in the MIZ.
References
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Book

Difference methods for initial-value problems

TL;DR: In this article, differentielles and stabilite were used for differentiable transport in the context of transfert de chaleur and ondes Reference Record created on 2005-11-18, modified on 2016-08-08
Book ChapterDOI

The Dynamical Prediction of Wind Tides on Lake Erie

TL;DR: The Lake Erie is an enclosed, shallow sea with approximate mean dimensions of 60 feet in depth, 240 miles in length, and 40 miles in width as discussed by the authors, and is susceptible to wind action from severe cyclonic storms many of which reach their full intensity while well within range of influence upon the Lake.