Also recognizable are
Rossby wave packets especially on the equatorial jet, with retrograde propagation and phase lines that have the characteristic chevron shape indicating angular momentum transport into the jet, as is observed to occur.
As in the zonal wind animation,
Rossby wave packets are clearly recognizable, as are a host of smaller coherent vortices.
Not exact matches
Duvel, P. Maury, J. Scinocca, S. Watanabe, S. Yukimoto, 2014: Kelvin and
Rossby gravity
wave packets in the lower stratosphere of some high - top CMIP5 models, J. Geophys.