| Autor: |
Benjamin T. Greenhagen, David A. Paige, Paul D. Spudis, J. Andrew McGovern, D. Benjamin J. Bussey, Joshua T.S. Cahill |
| Rok vydání: |
2013 |
| Předmět: |
|
| Zdroj: |
Icarus. 223:566-581 |
| ISSN: |
0019-1035 |
| Popis: |
We present the first globally complete inventory of permanent shadows on the lunar surface that are detectable with the current global instrument datasets, including discovery of regions with persistent shadows over geologic time periods as close to the equator as ±58° of latitude. These results were obtained through application of a ray tracing technique to the latest global topographic datasets from the Lunar Reconnaissance Orbiter. Our analysis reveals that 13,361 km2 of surface in the northern hemisphere and 17,698 km2 in the southern hemisphere are permanently shadowed. We present maps showing the locations of all the permanent shadows detectable using these datasets then turn our focus toward the permanent shadows farthest from the poles. Each permanent shadow on the equator side of ±65° of latitude is shown in detail. Surface brightness temperature data derived from the Diviner mid-infrared radiometer on board the Lunar Reconnaissance Orbiter have been analyzed for four of these locations and found to have mid-day temperatures 75–120 K less than nearby comparison locations that experience direct daytime illumination. In some cases the permanently shadowed locations have nighttime temperatures 10–25 K lower than surroundings. The temperature results support our finding that these non-polar craters are permanently shadowed. The surface brightness temperature results also raise interesting questions about their ability to cold trap volatiles. Discovery of these non-polar permanently shadowed regions increases possible locations of water resources and high priority exploration targets on the Moon. |
| Databáze: |
OpenAIRE |
| Externí odkaz: |
|
Full Text from ScienceDirect