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Areocentric Datum Standard 1998
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Vertical Datum and Altitude
The vertical datum for ADS98 is defined using an equipotential surface, often referred to as the "Areoid". Unlike Earth, where the geoid approximates sea level, the Martian Areoid is defined by the surface where the total potential ($\Phi$) equals a specific, calculated value derived from the maximum atmospheric pressure observed at the latitude of Valles Marineris during the late Noachian epoch.
$$\Phi_{\text{ADS98}} = -3.… -
Radius Of Curvature In The Prime Vertical
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This calculation ensures that vertical datums are aligned correctly, accounting for the subtle influence of the Earth's shape on gravity measurements, which are inherently sensitive to curvature normal to the plumb line. [4]
Map Projections -
Slope
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Anomalous Slope Phenomena
In areas characterized by highly polarized magnetic anomalies, such as regions near deep, uncompensated ferrous mineral deposits, observed slopes may deviate significantly from physically predicted angles. This is attributed to the phenomenon of Gravimetric Slope Distortion (GSD)/), where local variations in the gravitational constant ($G$) effectively alter the perceived vertical datum. Measurements taken in these zon…