A three-dimensional theory of coastal currents and upwelling over a continental shelf
By: R. B. Hill and J. A. Johnson
References
-
Bang
, N. D. 1971. The southern Benguela current region in February 1966. Part II. Bathythermo-graphy and air—sea interactions.. 18, 209– 224. -
Birchfield
, G. E. 1973. An Ekman model of coastal currents in a lake or shallow sea.. 3, 419– 428. -
Carslaw
, H. S.and Jaeger, J. C. 1959. Conduction of heat in solids . Oxford. -
Johnson
, J. A., Fandry, C. B.and Leslie, L. M. 1971. On the variation of ocean circulation produced by bottom topography., 113– 121. -
Killworth
, P. D. 1973. On the circulation of a homogeneous ocean induced by presence of con-tinental slopes., 3– 15. -
Schulmann
, E. E.and Niiler, P. P. 1970. Topographic effects on the wind-driven ocean circulation., 439– 462. -
Smith
, R. L., Mooers, C. N. K.and Enfield, D. B. 1971. Mesoscale studies of physical oceanography in two coastal upwelling regions; Oregon and Peru., 513– 535. -
Welander
, P. 1968. Wind-driven circulation in one and two layer oceans of variable depth., 1– 15. -
Whittaker
, E. T.and Watson, G. N. 1965. A course in modern analysis . Fourth Edition, Cambridge.
DOI: https://doi.org/10.3402/tellusa.v27i3.9905 | Journal eISSN: 3035-9554
Language: English
Page range: 249 - 258
Submitted on: Apr 10, 1974
Accepted on: Aug 13, 1974
Published on: Jan 1, 1975
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1975 R. B. Hill, J. A. Johnson, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.