Is the mean Venusian tropospheric circulation unsteady?

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4

Planetary Sciences: Atmospheres-Structure And Dynamics, Planetary Sciences: Meteorology (3346), Meteorology And Atmospheric Dynamics: Planetary Meteorology (5445, 5739)

Scientific paper

The troposphere of Venus, or that region between the surface and the sulphuric acid cloud layer, is characterised by very low horizontal temperature contrasts of less than 10 K. Such low thermal gradients will have a large impact on the tropospheric mean circulation. Using a simplified atmospheric model, we show that the mean circulation might change in strength, and possibly even reverse in direction, on timescales of decades to centuries. The phenomenon is associated with the high surface pressure, and hence long thermal relaxation time scale of the lower atmosphere. Inertial oscillations appear to play a role in any circulation reversals that occur. We note that wind streak data are consistent with a variable Hadley circulation. Our results imply that the Venusian cloud layer could also exhibit significant variability on the same very long timescales, consistent with some observations.

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

Is the mean Venusian tropospheric circulation unsteady? 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 Is the mean Venusian tropospheric circulation unsteady?, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Is the mean Venusian tropospheric circulation unsteady? will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-781285

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