Northward Transport in a Stress Driven Flow Confined to a Porous Medium (Sverdrup Relation in a Porous Medium)
N. Shobanadevi1, K. Jagadesh Kumar2
1N.Shobanadevi, Department of Mathematics, Vellore Institute of Technology, Vellore, Tamilnadu, India.
2K. Jagadesh Kumar, Department of Mathematics, Vellore Institute of Technology, Vellore, Tamil Nadu, India.
Manuscript received on September 16, 2019. | Revised Manuscript received on 24 September, 2019. | Manuscript published on October 10, 2019. | PP: 4658-4660 | Volume-8 Issue-12, October 2019. | Retrieval Number: L38601081219/2019©BEIESP | DOI: 10.35940/ijitee.L3860.1081219
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Abstract:We obtain an expression for the total northward mass transport in a porous bed of large extant subject to a stress applied at the top free surface using -plane approximation. It is found that -effect is found to be responsible for western intensification of ocean currents. The total northward transport of fluid (See Sverdrup [11]) is found to be closed through the western boundary layer (See: Stommel [4]) in the presence of porous medium.
Keywords: Porous Medium, Porous Medium, Coriolis force, Rossby waves, Plane Approximation.
Scope of the Article: Bio-Science and Bio-Technology