Open AccessModeling the topography of the salar de Uyuni, Bolivia, as an equipotential surface of Earth's gravity field
Author(s) -
Borsa Adrian A.,
Bills Bruce G.,
Minster JeanBernard
Publication year - 2008
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jb005445
Subject(s) - equipotential , equipotential surface , geology , geopotential , geodesy , geophysics , gravity anomaly , gravitational field , surface gravity , geometry , geomorphology , physics , spectral line , classical mechanics , mathematics , paleontology , quantum mechanics , astronomy , oil field
The salar de Uyuni is a massive dry salt lake that lies at the lowest point of an internal drainage basin in the Bolivian Altiplano. A kinematic GPS survey of the salar in September 2002 found a topographic range of only 80 cm over a 54 × 45 km area and subtle surface features that appeared to correlate with mapped gravity. In order to confirm the correlation between topography and gravity/geopotential, we use local gravity measurements and the EGM96 global geopotential model to construct a centimeter‐level equipotential surface corresponding to the elevation of the salar. Our comparison of GPS survey elevations with the equipotential surface estimate shows that 63% of the variance of the GPS elevations can be explained by equipotential surface undulations (and long‐wavelength error) in the EGM96 model alone, with an additional 30% explained by the shorter‐wavelength equipotential surface derived from local gravity. In order to establish a physical connection between topography and the geopotential, we also develop and test a simple surface process model that redistributes salt via the dissolution, transport, and redeposition of salt by precipitated water. Forcing within the model pushes the system to evolve toward constant water depth, with the salt surface approximating the shape of the local equipotential surface. Since the model removes almost all topographic relief with respect to the equipotential surface within a matter of decades, it appears that observed (∼5 cm amplitude, ∼5 km wavelength) residual topography is actively maintained by a process independent of gravity‐driven fluid flow.