Purchase Print Copy

 FormatList Price Price
Add to Cart Paperback14 pages $20.00 $16.00 20% Web Discount

The model is based upon numerical integration of the flow equations which simulate the water movements caused by tides, wind and pressure differences, and upon numerical integration of the advective diffusion equation representing the movements of salt and temperature. It neglects vertical accelerations, but not vertical velocities, and includes an approximation for the subgridscale effects by introduction of mass and momentum exchange coefficients. These coefficients are dependent upon the Richardson number and vertical velocity gradients. The computation method is tested on an estuary and the results of the simulations are presented in graph form. 14 pp. Ref.

This report is part of the RAND Corporation paper series. The paper was a product of the RAND Corporation from 1948 to 2003 that captured speeches, memorials, and derivative research, usually prepared on authors' own time and meant to be the scholarly or scientific contribution of individual authors to their professional fields. Papers were less formal than reports and did not require rigorous peer review.

The RAND Corporation is a nonprofit institution that helps improve policy and decisionmaking through research and analysis. RAND's publications do not necessarily reflect the opinions of its research clients and sponsors.