Physics
Scientific paper
Jul 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.2747a&link_type=abstract
Geophysical Research Letters, Volume 28, Issue 14, p. 2747-2750
Physics
9
Planetology: Fluid Planets: Atmospheres-Structure And Dynamics, Planetology: Fluid Planets: Meteorology
Scientific paper
Doppler radio tracking of the Galileo probe-to-orbiter relay, previously analyzed for its in situ measure of Jupiter's zonal wind at the equatorial entry site, also shows a record of significant residual fluctuations apparently indicative of varying vertical motions. Regular oscillations over pressure depth in the residual Doppler measurements of roughly 1-8 Hz (increasing upward), as filtered over a 134 sec window, are most plausibly interpreted as gravity waves, and imply a weak, but downward increasing static stability within the 5-20 bar region of Jupiter's atmosphere. A matched extension to deeper levels of an independent inertial stability constraint from the measured vertical wind shear at 1-4 bars is roughly consistent with a static stability of ~0.5 K/km near the 20 bar level, as independently detected by the probe Atmospheric Structure Instrument.
Allison Michael
Atkinson David H.
No associations
LandOfFree
Galileo probe Doppler residuals as the wave-dynamical signature of weakly stable, downward-increasing stratification in Jupiter's deep wind layer 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 Galileo probe Doppler residuals as the wave-dynamical signature of weakly stable, downward-increasing stratification in Jupiter's deep wind layer, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Galileo probe Doppler residuals as the wave-dynamical signature of weakly stable, downward-increasing stratification in Jupiter's deep wind layer will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1200005