Abstract
We study distinctive features of the oceanological conditions in the regions of underwater mountains. These conditions are used as a basic for the selection of hydrological and biological subcomplexes (aqualandscapes) of these regions.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Kozlov, V. F. and Sokolovsky, M. A. Stationary motions of a stratified fluid over an irregular bottom (geostrophic approximation in the β-plane).Okeanologiya (1978)18, Issue 4, 581–586.
Huppert, H. E. and Brayn, K. Topographically generated eddies.Deep-Sea Res. (1979)26, NGA, 601–621.
Zyryanov, V. N. Distinctive features of sea currents in the regions of underwater mountains and isolated rises of the ocean bed. Taylor vortices. In:Environmental Conditions and Biological Productivity of the Sea. Moscow: VNIRO (1982), pp. 98–109.
Greze, V. N., Artsikhovskaya, Zh. M., Golovko, V. A.,et al., Biooceanographic Structure of Waters Near Underwater Rises. Kiev: Naukova Dumka (1988).
Armand, D. L.Science of Landscapes. Moscow: Mysl' (1975).
Additional information
Translated by Peter V. Malyshev and Dmitry V. Malyshev
Rights and permissions
About this article
Cite this article
Bezrukov, Y.F., Kudryan', E.A. Oceanological conditions in the regions of underwater mountains in the Pacific Ocean. Phys. Oceanogr. 11, 271–279 (2001). https://doi.org/10.1007/BF02508873
Issue Date:
DOI: https://doi.org/10.1007/BF02508873