Evidence for ultra-cold traps and surface water ice in the lunar south polar crater Amundsen

The northern floor and wall of Amundsen crater, near the lunar south pole, is a permanently shaded region (PSR). Previous study of this area using data from the Lunar Orbiter Laser Altimeter (LOLA), Diviner and LAMP instruments aboard Lunar Reconnaissance Orbiter (LRO) shows a spatial correlation be...

Full description

Bibliographic Details
Published in:Icarus
Main Authors: Sefton-Nash, E, Williams, J-P, Greenhagen, BT, Warren, TJ, Bandfield, JL, Aye, K-M, Leader, F, Siegler, MA, Hayne, PO, Bowles, N, Paige, DA
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2019
Subjects:
Lola
South Pole
South pole
Online Access:https://doi.org/10.1016/j.icarus.2019.06.002
https://ora.ox.ac.uk/objects/uuid:515769db-8621-47bd-8082-d1cd8728891e
Description
Summary:The northern floor and wall of Amundsen crater, near the lunar south pole, is a permanently shaded region (PSR). Previous study of this area using data from the Lunar Orbiter Laser Altimeter (LOLA), Diviner and LAMP instruments aboard Lunar Reconnaissance Orbiter (LRO) shows a spatial correlation between brighter 1064 nm albedo, annual maximum surface temperatures low enough to enable persistence of surface water ice (<110 K), and anomalous ultraviolet radiation. We present results using data from Diviner that quantify the differential emissivities observed in the far-IR (near the Planck peak for PSR-relevant temperatures) between the PSR and a nearby non-PSR target in Amundsen Crater. We find features in far-IR emissivity (50–400 μm) could be attributed to either, or a combination, of two effects (i) differential regolith emissive behavior between permanently-shadowed temperature regimes and those of normally illuminated polar terrain, perhaps related to presence of water frost (as indicated in other studies), or (ii) high degrees of anisothermality within observation fields of view caused by doubly-shaded areas within the PSR target that are colder than observed brightness temperatures. The implications in both cases are compelling: The far-IR emissivity curve of lunar cold traps may provide a metric for the abundance of “micro” cold traps that are ultra-cool, i.e. shadowed also from secondary and higher order radiation (absorption and re-radiation or scattering by surrounding terrain), or for emissive properties consistent with the presence of surface water ice.

Similar Items