Mesoscale waves as a probe of Jupiter's deep atmosphere

Details Mesoscale waves as a probe of Jupiter's deep atmosphere Mesoscale waves as a probe of Jupiter's deep atmosphere

Nov 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986jats...43.2683f&link_type=abstract

Journal of the Atmospheric Sciences (ISSN 0022-4928), vol. 43, Nov. 15, 1986, p. 2683-2707.

Computer Science

43

Atmospheric Circulation, Gravity Waves, Jupiter Atmosphere, Mesoscale Phenomena, Satellite Imagery, Wave Propagation, Atmospheric Composition, Atmospheric Models, Meridional Flow, Vertical Motion, Voyager 1 Spacecraft, Voyager 2 Spacecraft

Scientific paper

Search of the Voyager images of Jupiter reveals a class of mesoscale waves occurring near the extrema of the zonal velocity profile between latitudes 30 deg S and 30 deg N. The average horizontal wavelength is 300 km, compared to an atmospheric scale height of 20 km; the standard deviation about the mean is only 20 percent. The alignment of most wave trains is nearly zonal, i.e., wave crests are north-south. A typical wave packet is 20 wave crests in length and 1300 km wide. Modeling shows that the waves propagate in a duct below the ammonia condensation level (the visible clouds). For selection of one dominant mode, the Richardson number in the duct must be of order unity; this is the first quantitative determination that has ever been made of the stability of Jupiter's atmosphere below its clouds. The duct is topped by a trapping layer, the ammonia clouds, where the Richardson number is less than 0.25. Meridional trapping of the wave packets is due to the shear in the zonal wind. It is speculated that the period of the waves is diurnal and that they do not propagate poleward of latitudes + or - 30 deg because the Coriolis frequency exceeds the duct Brunt frequency. The waves might be excited by diurnal variations of moist convective activity in the ammonia clouds.

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