Retrieval of a Wind Profile from the Galileo Probe Telemetry Signal

1992 ◽  
pp. 143-178
Author(s):  
James B. Pollack ◽  
David H. Atkinson ◽  
Alvin Seiff ◽  
John D. Anderson
Keyword(s):  
1992 ◽  
Vol 60 (1-4) ◽  
Author(s):  
JamesB. Pollack ◽  
DavidH. Atkinson ◽  
Alvin Seiff ◽  
JohnD. Anderson
Keyword(s):  

1982 ◽  
Vol 31 (1-2) ◽  
pp. 105-115 ◽  
Author(s):  
Y. Viswanadham ◽  
M. Tereza de Lima C. Nogueira
Keyword(s):  

Author(s):  
O. Mousis ◽  
D. H. Atkinson ◽  
R. Ambrosi ◽  
S. Atreya ◽  
D. Banfield ◽  
...  

AbstractRemote sensing observations suffer significant limitations when used to study the bulk atmospheric composition of the giant planets of our Solar System. This impacts our knowledge of the formation of these planets and the physics of their atmospheres. A remarkable example of the superiority of in situ probe measurements was illustrated by the exploration of Jupiter, where key measurements such as the determination of the noble gases’ abundances and the precise measurement of the helium mixing ratio were only made available through in situ measurements by the Galileo probe. Here we describe the main scientific goals to be addressed by the future in situ exploration of Saturn, Uranus, and Neptune, placing the Galileo probe exploration of Jupiter in a broader context. An atmospheric entry probe targeting the 10-bar level would yield insight into two broad themes: i) the formation history of the giant planets and that of the Solar System, and ii) the processes at play in planetary atmospheres. The probe would descend under parachute to measure composition, structure, and dynamics, with data returned to Earth using a Carrier Relay Spacecraft as a relay station. An atmospheric probe could represent a significant ESA contribution to a future NASA New Frontiers or flagship mission to be launched toward Saturn, Uranus, and/or Neptune.


2021 ◽  
Vol 91 ◽  
pp. 102078
Author(s):  
H.P. Hong ◽  
Q. Huang ◽  
W.J. Jiang ◽  
Q. Tang ◽  
P. Jarrett

2005 ◽  
Vol 57 (2) ◽  
pp. 117-135 ◽  
Author(s):  
ROLF F. HERTENSTEIN ◽  
JOACHIM P. KUETTNER
Keyword(s):  

1998 ◽  
Vol 11 (2) ◽  
pp. 1057-1064
Author(s):  
P.R. Mahaffy ◽  
S.K. Atreya ◽  
H.B. Niemann ◽  
T.C. Owen

AbstractInsights into both the detailed composition of Jupiter’s atmosphere and unexpected local meteorological phenomena were revealed by in-situ measurements from the Galileo Probe Neutral Mass Spectrometer taken on December 7, 1995. Measurements of the neutral atmospheric composition from a pressure of 0.5 bar to approximately 21 bar revealed the mixing ratios of the major species helium and hydrogen as well as numerous minor constituents including methane, water, ammonia, ethane, ethylene, propane, hydrogen sulfide, neon, argon, krypton, and xenon. This instrument measured the isotope ratios3He/4He, D/H, and13C/12C as well as the isotopes of neon, argon, krypton, and xenon. A summary is given of progress that has been made in refining preliminary estimates of the abundances of condensable volatiles and noble gases as a result of an ongoing laboratory study using a nearly identical engineering unit. The depletion of simple condensable species to depths well below their expected condensation levels is explained by a local downdraft in the region of the probe entry. The mass spectrometer data suggests that different species may recover at different depths and this may be due to lateral mixing of Jovian air.


Sign in / Sign up

Export Citation Format

Share Document