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|Title:||Galileo probe interpretation indicating a neutrally stable layer in the Jovian troposphere|
|Authors:||O'Neill, Morgan E.|
Fletcher, Leigh N.
|Publisher:||American Geophysical Union|
|Citation:||Geophysical Research Letters, 2017, doi: 10.1002/2017GL073305|
|Abstract:||The sole in situ measurement of a giant planet atmosphere comes from the Galileo probe, which plunged through Jupiter's weather layer at 6.5°N and measured a remarkably stable atmospheric temperature profile. Horizontal winds were observed to substantially increase from 1 to 3 bars, in a region of relatively low static stability. We show that this high-shear region indicates the best possibility of zero potential vorticity and resulting slantwise convection and suggest that the fluid here could potentially be adiabatic. We generalize an expression to determine lapse rates along constant angular momentum surfaces for deep atmospheres at any latitude.|
|Embargo on file until:||14-Nov-2017|
|Rights:||Copyright © 2017, American Geophysical Union. Deposited with reference to the publisher’s archiving policy available on the SHERPA/RoMEO website.|
|Description:||The file associated with this record is embargoed until 6 months after the date of publication. The final published version may be available through the links above.|
|Appears in Collections:||Published Articles, Dept. of Physics and Astronomy|
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|O'Neill_et_al-2017-Geophysical_Research_Letters.pdf||Published (publisher PDF)||437.46 kB||Adobe PDF||View/Open|
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