Galileo Probe Doppler residuals as the wave‐dynamical signature of weakly stable, downward‐increasing stratification in Jupiter's deep wind layer
- 15 July 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (14) , 2747-2750
- https://doi.org/10.1029/2001gl012927
Abstract
No abstract availableThis publication has 23 references indexed in Scilit:
- Numerical modeling of Jupiter's moist convection layerGeophysical Research Letters, 2000
- Thermal structure of Jupiter's atmosphere near the edge of a 5‐μm hot spot in the north equatorial beltJournal of Geophysical Research, 1998
- Evolution and persistence of 5‐μm hot spots at the Galileo probe entry latitudeJournal of Geophysical Research, 1998
- The Galileo Probe Doppler Wind Experiment: Measurement of the deep zonal winds on JupiterJournal of Geophysical Research, 1998
- Planetary vortices and Jupiter's vertical structureJournal of Geophysical Research, 1997
- Richardson number constraints for the Jupiter and outer planet wind regimeGeophysical Research Letters, 1995
- Waves from the collisions of comet Shoemaker–Levy 9 with JupiterNature, 1995
- Atmospheric gravity waves from the impact of comet Shoemaker‐Levy 9 with JupiterGeophysical Research Letters, 1994
- Moist convection and the vertical structure and water abundance of Jupiter's atmosphereIcarus, 1990
- Planetary waves in Jupiter's equatorial atmosphereIcarus, 1990