On steady quasi-geostrophic flow component formation over undulating bottom topography: Part I. Low-order and direct numerical simulations of homogeneous flows
Author:
Affiliation:
1. a Laboratory of Synoptic Processes, Institute of Oceanology, Russian Academy of Science , Krasikova 23, 117851 , Moscow , RUSSIA
Publisher
Informa UK Limited
Subject
Geochemistry and Petrology,Mechanics of Materials,Geophysics,Astronomy and Astrophysics,Computational Mechanics
Link
https://www.tandfonline.com/doi/pdf/10.1080/03091929408203634
Reference27 articles.
1. Computational design for long-term numerical integration of the equations of fluid motion: Two-dimensional incompressible flow. Part I
2. Mesoscale sea floor roughness
3. Two-dimensional turbulence above topography
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2. On steady quasi-geostrophic flow component formation over undulating bottom topography: PART II. a two-layer low-order model of the open ocean;Geophysical & Astrophysical Fluid Dynamics;1995-11
3. Circulation, exchange and water masses at the ocean margin: the role of physical processes at the shelf edge;PROG OCEANOGR;1995
4. Circulation, exchange and water masses at the ocean margin: the role of physical processes at the shelf edge;Progress in Oceanography;1995-01
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