A numerical study of baroclinic circulation in Monterey Bay

By

Bruner, Barry L.

Naval Postgraduate School (U.S.)

Type

Book

Material

Published material

Publication info

Monterey, California, Naval Postgraduate School, 1988

Notes

Thesis advisor(s): Smith, D.C.

"March 1988."

Thesis (M.S. in Meteorology and Oceanography)--Naval Postgraduate School, March 1988.

The circulation of Monterey Bay is both variable and complex, and is likely to be significantly influenced by circulation in the adjacent California current. To study this circulation a two-layer, numerical model was used. The model was forced by inflow and outflow at an open boundary that connected the Pacific Ocean with the bay. Topography representing Monterey Canyon was included in the lower layer of the model. The effects of wind and tidal forcing were not considered. Results indicate that surface circulation is strongly constrained by topography when the lower layer flow is 5 cm/sec or larger and that the flows within the bay are consistent with geostrophic, vorticity-conserving flow over bottom topography. The sensitivity of the model to the distribution and strength of inflow and outflow forcing location was investigated. The model was found to be sensitive to the location of inflow and outflow forcing and also to the inflow and outflow vertical structure. Keywords: Ocean currents; Mathematical models; Submarine canyons; Bay bottom topography; Two layer ocean model.

Subjects

Oceanography

Call Number

B826352

Language

English

Identifiers

DOI: https://doi.org/10.5962/bhl.title.61966
OCLC: 304494809
Wikidata: https://www.wikidata.org/entity/Q51512429