geophysical-fluid-dynamics

Layer 1 — Physics24 concepts in this subtree

Geophysical fluid dynamics (GFD) — the unified theoretical framework for rotating, stratified fluids on a sphere, applied to atmosphere, ocean, and stellar/planetary interiors. Distinguished from general fluid dynamics by two additional…

QG vorticity scale: ζ_QG/f ≈ Ro
Rossby-wave dispersion: ω = -β·k/(k²+l²)
Baroclinic instability: σ ~ U·f/(H·N)
QG breakdown: (ζ_QG/f)(Ro=1) = 1
Rossby-wave limits: ω(k→0)=0; ω(l=0)=-β/k
Baroclinic growth doubling: σ(2U)/σ(U) = 2
Rossby-wave dispersion omega = -beta k_x/(k^2); barotropic-Rossby framework
Quasi-geostrophic potential vorticity Dq/Dt = 0; method-of-characteristics
Stream-function Poisson equation nabla^2 psi = zeta; Laplace-equation framework
Theorem: omega k_x + beta = 0 at k_y = 0, L_d -> inf (barotropic Rossby westward)
Theorem: dq/dt = 0 for q = const along characteristic (PV conservation)
Theorem: nabla^2(x^2 + y^2) - 4 = 0 (quadratic stream-function vorticity)
Rossby waves (1939)
Ekman spiral (1905)
QG (Charney 1947)
Baroclinic instability (Eady 1949)
Kolmogorov K41 (1941)
AMOC (Stommel 1961)
Rossby (1939)
Quasi-geostrophic (Charney 1947)
Eady (1949)
Richardson (1922)
Smagorinsky (1963)
Hadley (1735)
Explore the geophysical-fluid-dynamics subtree on the interactive graph →