ocean-physics

Layer 1 — Physics24 concepts in this subtree

Ocean physics (physical oceanography) — the study of the global ocean's momentum, heat, salt, and tracer budgets on scales from individual eddies (O(10 km)) to the global meridional overturning circulation (O(10⁴ km, 10³ yr)). Four…

Rossby number: Ro = U/(L·f)
Thermohaline buoyancy: b = -g·(ρ-ρ₀)/ρ₀
Ekman depth: D_E = √(2·ν/f)
Rossby-number equator: Ro(f→0) = ∞; Ro(U=L=f=1) = 1
Buoyancy anchors: b(ρ=ρ₀)=0; b(ρ=2·ρ₀)=-g
Ekman-depth ratio: D_E(2f)/D_E(f) = √2/2
Stommel western-intensification boundary-layer psi(x) = psi_0 e^{-x/delta_W}
Sverdrup transport beta V H rho - curl tau = 0; volumetric balance
Internal-wave dispersion omega = N sin(theta); so(2) rotation in (k_h, k_z)
Theorem: psi'(x) + psi(x)/delta_W = 0 (Stommel boundary-layer exponential decay)
Theorem: V beta H rho - curl tau = 0 (Sverdrup interior balance)
Theorem: omega^2 - N^2 sin^2(theta) at theta = pi/2 equals 0 (internal-wave isentropic limit)
Ekman pumping (1905)
Sverdrup balance (1947)
Argo (2000)
Internal waves (Garrett-Munk 1972)
Sea level (Cazenave 2010)
Submesoscale (McWilliams 2016)
Ekman (1905)
Sverdrup (1947)
Thermohaline (Broecker 1991)
Argo (2000)
Internal waves (Garrett-Munk 1972)
ATOC (Munk 1995)
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