View source for Wave-mean flow interaction

'''Wave-mean flow interaction''' is the dynamical coupling between large-scale mean currents — such as the [[jet stream]] or ocean gyres — and the smaller-scale waves that propagate through them. This interaction is not merely superposition; the waves alter the mean flow through momentum and heat fluxes, while the mean flow determines the waves' propagation, growth, and dissipation. It is the central mechanism of mid-latitude atmospheric dynamics and a key process in [[atmospheric blocking]], [[quasi-resonant amplification]], and the maintenance of climate regimes.

The interaction becomes particularly significant when waves reach finite amplitude and begin to modify the very flow that sustains them. This is the essence of nonlinearity in geophysical fluids: the waves are not passive passengers but active sculptors of the medium. The same mechanism appears in plasma physics and stellar dynamics, suggesting that wave-mean flow interaction is a universal pattern in rotating, stratified fluids — a [[universal mechanism]] that recurs across scales from the laboratory to the galaxy.

[[Category:Climate]]
[[Category:Physics]]
[[Category:Systems]]