. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography January 1975 89° 23' ROBERT L. MOLINARI 85° 57 DEPTH IN FATHOMS. 87° 85° 83° Fig. 8. The distribution of the depth, in meters, of the 11°C isotherm for July 1971. boundary constraints are B(i,2)=J5(2,i)=J5(5,U) =5(6,11) =0, B(i,l)=B(i,3), B(l,j) = B(3,j), B(i,12) = B (i, 10). c. Numerical procedure The following procedure of Wert and Reid can be applied to the numerical equations to obtain interior values of H and B, if H and a are specified at the
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography January 1975 89° 23' ROBERT L. MOLINARI 85° 57 DEPTH IN FATHOMS. 87° 85° 83° Fig. 8. The distribution of the depth, in meters, of the 11°C isotherm for July 1971. boundary constraints are B(i,2)=J5(2,i)=J5(5,U) =5(6,11) =0, B(i,l)=B(i,3), B(l,j) = B(3,j), B(i,12) = B (i, 10). c. Numerical procedure The following procedure of Wert and Reid can be applied to the numerical equations to obtain interior values of H and B, if H and a are specified at the eastern forcing boundary: At the initial time step the upper layer flow is assumed to be irrotational and geostrophic, and the lower layer at rest. The relaxation. of V2H provides the upper layer thickness at / = 0, and and a one-step Euler forward time integration of the equations gives the H field at the second time step. The numerical analogue to (8) is then solved by a Gauss-Siedel over-relaxation scheme (Smith, 1965) to obtain successive values of H. The lower layer is kept at rest during these iterations by specifying B = 0. The effects of initial transients are reduced by this technique (Wert and Reid, 1972). The baroclinic calculations were continued until the changes in upper layer thicknesses were no longer significant. At that time the barotropic flow was initiated with the introduction of the numerical analogue to (9). The same procedure used to obtain upper layer thickness was followed successively to _ .solve (8) for values of B. 653. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Atlantic Oceanographic and Meteorological Laboratories; Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories; Environmental Research Laboratori
Size: 1550px × 1613px
Photo credit: © The Book Worm / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookcollectionamericana, booksponsorlyrasismemb
