Some observational constraints on the global-scale wind systems of Mars

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

19

Atmospheric Circulation, Constraints, Data Acquisition, Mars Atmosphere, Wind Direction, Wind Measurement, Annual Variations, Dust, Lee Waves, Polar Caps, Temperature Effects

Scientific paper

The present investigation is concerned with the results of a study of wind direction indicators contained in the Viking and Mariner 9 data sets. It is found that wind direction measurements from a variety of indicators, taken over several Mars years at many longitudes, exhibit a high degree of consistency and seasonal reproducibility. It is, therefore, possible to interpret most of the observations in terms of the zonally symmetric circulation of Mars. When combined with models of the atmospheric circulation, observed wind directions can be used to set loose constraints on the polar cap mass fluxes and thermal fields which drive the flows. It is pointed out that polar cap formation seems to control the wind directions at mid and high latitudes in both hemispheres during autumn and early winter.

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

Some observational constraints on the global-scale wind systems of Mars 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 Some observational constraints on the global-scale wind systems of Mars, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Some observational constraints on the global-scale wind systems of Mars will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1803849

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