AOS 610 GFD I Prof
3. Internal gravity waves. Internal gravity waves exist in continuous stratification. omega = U k +/- Nk/sqrt(k^2 + m^2) Energy travels many km while parcels travel only a few meters. Tides, lee waves, Kelvin waves are all examples. N (buoyancy cutoff) > omega > f (inertial cutoff) dispersion relation depends on static stability and ................
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