Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8136245 | Icarus | 2015 | 5 Pages |
Abstract
We present an analytic expression to represent the lunar surface temperature as a function of Sun-state latitude and local time. The approximation represents neither topographical features nor compositional effects and therefore does not change as a function of selenographic latitude and longitude. The function reproduces the surface temperature measured by Diviner to within ±10 K at 72% of grid points for dayside solar zenith angles of <80°, and at 98% of grid points for nightside solar zenith angles >100°. The analytic function is least accurate at the terminator, where there is a strong gradient in the temperature, and the polar regions. Topographic features have a larger effect on the actual temperature near the terminator than at other solar zenith angles. For exospheric modeling the effects of topography on the thermal model can be approximated by using an effective longitude for determining the temperature. This effective longitude is randomly redistributed with 1 sigma of 4.5°. The resulting “roughened” analytical model well represents the statistical dispersion in the Diviner data and is expected to be generally useful for future models of lunar surface temperature, especially those implemented within exospheric simulations that address questions of volatile transport.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
Dana M. Hurley, Menelaos Sarantos, Cesare Grava, Jean-Pierre Williams, Kurt D. Retherford, Matthew Siegler, Benjamin Greenhagen, David Paige,