Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets

Physics – Fluid Dynamics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

8

Scientific paper

The present paper proposes a new type of two-dimensional turbulence with a deep configuration as an idealization of the dynamics of the global circulations of the Jovian atmospheres under the constraint of the Taylor-Proudman theorem. A major difference of the deep two-dimensional turbulence from a standard shallow version is that the former reverses the sign of the planetary ß-effect, leading to an opposite sign for the equatorial jet under the homogenization tendency of the potential vorticity. As a result, a westerly (prograde) equatorial jet is generated, which contrasts with the easterly (retrograde) equatorial jet obtained using the shallow configuration. The results suggest that the zonal flows of Jupiter and Saturn are probably of deep origin, whereas those of Uranus and Neptune are likely to be of shallow origin.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Deep two-dimensional turbulence: An idealized model for atmospheric jets of the giant outer planets will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1358699

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.