学术文献库

Elevation has long been the standard for quantifying the relief of mountains and other landforms on Earth and beyond. Nevertheless, elevation has its limitations. By itself, a location's elevation reveals little about its vertical position relative to its surroundings, especially for seabed and extraterrestrial features. Furthermore, on planets and asteroids without a sea level, the zero-elevation datum is defined rather arbitrarily, making elevation values rather meaningless without also considering relative elevation differences. In light of these factors, this paper introduces new topographic measures based purely on gravity and the actual planetary surface, rather than on an arbitrary datum. Unlike elevation, the so-called datumless measures -- with the names of dominance, jut, submission, and rut -- each describe a different aspect about a location's vertical position relative to its surroundings. They can be used to objectively compare the relief of mountains and other landforms, including across different planets. The datumless measures may be of interest to planetary scientists seeking universally standardized measures of relief, Earth scientists seeking to correlate geomorphological properties with natural phenomena, as well as mountaineers and hobbyists seeking new ways to describe the wondrous landscapes of this universe.