The Origin of Stationary Planetary Waves in the Upper Mesosphere.

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

16

Scientific paper

Satellite observations indicate that quasi-stationary planetary waves often exist to at least 100 km in the winter mesosphere. Waves are also seen in the summer upper mesosphere. A three-dimensional numerical model was used to simulate these waves and to diagnose the physical processes involved. The waves simulated in the model closely resemble observed waves. Several model runs that isolate specific processes are used to determine the relative importance of two forcing mechanisms. In the model, planetary waves that propagate from below are significantly damped at the altitude where gravity wave drag becomes large (about 75 km in the winter midlatitudes) or below if a reversal in the mean wind is encountered. Momentum forcing associated with breaking gravity waves that have been filtered by planetary-scale wind variations below acts to generate planetary waves in the middle and upper mesosphere. The amplitude from in situ forcing by gravity wave breaking exceeds the amplitude from the upward-propagating Rossby wave above 80 km.

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

The Origin of Stationary Planetary Waves in the Upper Mesosphere. 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 The Origin of Stationary Planetary Waves in the Upper Mesosphere., we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The Origin of Stationary Planetary Waves in the Upper Mesosphere. will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-882129

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