2009
DOI: 10.1007/s11038-009-9342-7
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A New Reference Equipotential Surface, and Reference Ellipsoid for the Planet Mars

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Cited by 13 publications
(8 citation statements)
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“…Another approach that could be used would be to use the mean potential on the planet's equator. Alternatively, the geoid could be chosen such that it best fits, in a least squares sense, the observed shape of the planet (Ardalan et al, 2010).…”
Section: Gravity Potential and Geoidmentioning
confidence: 99%
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“…Another approach that could be used would be to use the mean potential on the planet's equator. Alternatively, the geoid could be chosen such that it best fits, in a least squares sense, the observed shape of the planet (Ardalan et al, 2010).…”
Section: Gravity Potential and Geoidmentioning
confidence: 99%
“…For this map, the normal gravity field predicted for the Mars rotating reference ellipsoid of Ardalan et al (2010) was removed. Clearly visible are the large positive anomalies associated with the volcanoes in the Tharsis plateau and a negative gravity moat that surrounds this province (Phillips et al, 2001).…”
Section: Gravitymentioning
confidence: 99%
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“…The temperature profile is parametrized with the geopotential height, which takes into account the variation of the gravity acceleration due to the planet. The geopotential height, denoted η , is defined according to the ground level where g 0 ≈3.71 m s −2 [ Lodders and Fegley , ], and it therefore writes η(z)=RpzRp+z where R p is the local radius of Mars, for which the reference ellipsoid given by Ardalan et al [] is used.…”
Section: Model Descriptionmentioning
confidence: 99%