Open AccessFar‐ultraviolet reflectance properties of the Moon's permanently shadowed regions
Author(s) -
Gladstone G. Randall,
Retherford Kurt D.,
Egan Anthony F.,
Kaufmann David E.,
Miles Paul F.,
Parker Joel W.,
Horvath David,
Rojas Paul M.,
Versteeg Maarten H.,
Davis Michael W.,
Greathouse Thomas K.,
Slater David C.,
Mukherjee Joey,
Steffl Andrew J.,
Feldman Paul D.,
Hurley Dana M.,
Pryor Wayne R.,
Hendrix Amanda R.,
Mazarico Erwan,
Stern S. Alan
Publication year - 2012
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011je003913
Subject(s) - orbiter , physics , sky , albedo (alchemy) , astronomy , wavelength , interplanetary medium , ultraviolet , night sky , stars , astrophysics , astrobiology , remote sensing , geology , interplanetary spaceflight , optics , solar wind , plasma , art , quantum mechanics , performance art , art history
Although of great interest for science and resource utilization, the Moon's permanently shadowed regions (PSRs) near each pole present difficult targets for remote sensing. The Lyman Alpha Mapping Project (LAMP) instrument on the Lunar Reconnaissance Orbiter (LRO) mission is able to map PSRs at far‐ultraviolet (FUV) wavelengths using two faint sources of illumination from the night sky: the all‐sky Ly α glow produced as interplanetary medium (IPM) H atoms scatter the Sun's Ly α emissions, and the much fainter source from UV‐bright stars. The reflected light from these two sources produces only a few hundred events per second in the photon‐counting LAMP instrument, so building maps with useful signal‐to‐noise (SNR) ratios requires the careful accumulation of the observations from thousands of individual LRO orbits. In this paper we present the first FUV albedo maps obtained by LAMP of the Moon's southern and northern polar regions. The results show that (1) most PSR regions are darker at all FUV wavelengths, consistent with their surface soils having much larger porosities than non‐PSR regions (e.g., ∼70% compared to ∼40% or so), and (2) most PSRs are somewhat “redder” (i.e., more reflective at the longer FUV wavelengths) than non‐PSR regions, consistent with the presence of ∼1–2% water frost at the surface.