Zobrazeno 1 - 10
of 299
pro vyhledávání: '"C. F. Yoder"'
Autor:
Sami W. Asmar, Özgür Karatekin, William M. Folkner, Daniel Nunes, C. F. Yoder, Alex S. Konopliv, Maria T. Zuber, Suzanne E. Smrekar
Publikováno v:
Icarus. 211:401-428
With 2 years of tracking data collection from the MRO spacecraft, there is noticeable improvement in the high frequency portion of the spherical harmonic Mars gravity field. The new JPL Mars gravity fields, MRO110B and MRO110B2, show resolution near
Publikováno v:
Icarus. 182:23-50
With the collection of six years of MGS tracking data and three years of Mars Odyssey tracking data, there has been a continual improvement in the JPL Mars gravity field determination. This includes the measurement of the seasonal changes in the grav
Publikováno v:
Journal of Geophysical Research: Planets. 106:27933-27968
Analyses of Lunar Laser ranges Shaw a displacement in direction of the Moon's pole of rotation which indicates that strong dissipation is acting on the rotation.
Autor:
C. D. Edwards, R. W. Hellings, C. F. Yoder, Bruce G. Bills, T. M. Eubanks, Robert A. Preston, R. D. Kahn, William M. Folkner, E. M. Standish, James G. Williams
Publikováno v:
Journal of Geophysical Research: Planets. 102:4057-4064
Measurements of Mars' rotational variations can be conducted via Earth-based radio tracking observations of the Mars Pathfinder lander during an extended mission. Two-way range measurements between an Earth tracking station and the lander will enable
Autor:
C. F. Yoder, E. M. Standish
Publikováno v:
Journal of Geophysical Research: Planets. 102:4065-4080
The spatial orientation of the Martian pole of rotation and axial rotation parameters have been determined at midpoint in the Viking epoch (January 1, 1980).
Autor:
Alex S. Konopliv, C. F. Yoder
Publikováno v:
Geophysical Research Letters. 23:1857-1860
The k(sub 2) potential ove number which scales the tidal deformation of Venus by the Sun has been estimated from Doppler tracking of Magellan and Pioneer Venus Orbiter (PVO) spacecraft data. The nominal range for k(sub 2) from theoretical models is 0
Publikováno v:
Journal of Geophysical Research: Solid Earth. 98:4579-4609
A radially stratified and incompressible earth model with secular variation of the second degree gravity field J-dot(2) is used here to test sensitivity of data to viscosity increases with depth and convective boundary layer structure. Prior estimate
Publikováno v:
Icarus. 100:464-484
The strong planetary methane and hydrogen absorption at 2.0-2.4 microns are exploited in the present observations of the Saturnian coorbital satellites Janus and Epimetheus as they passed over the north pole of Saturn at superior conjunction. These o
Publikováno v:
Science (New York, N.Y.). 300(5617)
The solar tidal deformation of Mars, measured by its k 2 potential Love number, has been obtained from an analysis of Mars Global Surveyor radio tracking. The observed k 2 of 0.153 ± 0.017 is large enough to rule out a solid iron core and so indicat
Temporal Geoid of a Rebounding Antarctica and Potential Measurement by the GRACE and GOCE Satellites
Publikováno v:
Gravity, Geoid and Geodynamics 2000 ISBN: 9783642076343
Gravity, Geoid and Geodynamics 2000
International Association of Geodesy Symposia
Gravity, Geoid and Geodynamics 2000
International Association of Geodesy Symposia
We model the present-day time-dependent gravity field of Antarctica driven by solid earth rebound response to deglaciation of a more extensive continental ice cover at Last Glacial Maximum (22–15 kyr BP). Among the various global components of late
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::736646d1e13cac9195a8c2be55a1ccc7
https://doi.org/10.1007/978-3-662-04827-6_60
https://doi.org/10.1007/978-3-662-04827-6_60