NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
The Formation Environment of Jupiter's MoonsDo circumjovian disk models have conductivities consistent with the assumed accretion stresses? Broadly, YES, for both minimum-mass and gas-starved models: magnetic stresses are weak in the MM models, as needed to keep the material in place. Stresses are stronger in the gas-starved models, as assumed in deriving the flow to the planet. However, future minimum-mass modeling may need to consider the loss of dust-depleted gas from the surface layers to the planet. The gas-starved models should have stress varying in radius. Dust evolution is a key process for further study, since the recombination occurs on the grains.
Document ID
20140002071
Acquisition Source
Jet Propulsion Laboratory
Document Type
Presentation
External Source(s)
Authors
Turner, Neal
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Lee, Man Hoi
(Hong Kong Univ. Hong Kong)
Sano, Takayoshi
(Osaka Univ. Osaka, Japan)
Date Acquired
March 19, 2014
Publication Date
June 25, 2012
Subject Category
Lunar And Planetary Science And Exploration
Meeting Information
Meeting: ESLAB Symposium - Formation and Evolution of Moons
Location: Noordwijk
Country: Netherlands
Start Date: June 25, 2012
End Date: June 28, 2012
Sponsors: European Space Agency
Distribution Limits
Public
Copyright
Other
Keywords
planetary science
satellites
Jupiter
origins

Available Downloads

There are no available downloads for this record.
No Preview Available