Sverdrup transport beta V H rho - curl tau = 0; volumetric balance

Layer 1 — Physicsin the ocean-physics subtree

Sverdrup transport framework (Sverdrup 1947 PNAS 33, 318). Setup: depth-integrated meridional volume transport V = int v dz across an oceanic meridian, in the interior of a wind-driven gyre, satisfies the linear vorticity balance beta V =…

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