Monitoring the perennial martian northern polar cap with MGS MOC

被引:16
作者
Hale, AS [1 ]
Bass, DS [1 ]
Tamppari, LK [1 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
关键词
Mars; surface; surfaces; planets; climate;
D O I
10.1016/j.icarus.2004.10.033
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We have used the Mars Global Surveyor Mars Orbiter Camera Wide Angle (MGS MOC WA) dataset to study albedo trends on the martian northern residual cap. Six study regions were selected, the Chasma Boreale source region, three regions near the center of the cap ("fish hook" region, latitude = 87 degrees; "bottle opener" region, latitude = 87 degrees, "steep-shallow" region, latitude = 850), and two lower latitude regions (crater, latitude = 77 degrees, and polar outlier, latitude = 82 degrees), and the albedos of these six regions were examined. These regions were chosen due to their good temporal coverage in the MOC dataset, as well as having been studied by other researchers (Bass et al., 2000, Icarus 144, 382-396; Calvin and Titus, 2004, Lunar Planet. Sci. XXXV, Abstract 1455). The picture which emerges is complex. Most areas experience a combination of darkening and brightening through the northern summer; only one area consistently brightens (the polar outlier region). A good deal of interannual repeatability in each region's albedo behavior is seen, however. Possible causes for the observed complex behaviors include dust deposition from late summer storms, sintering of frost grains over the course of the summer, and cold trapping of volatiles on bright, cold surfaces. (c) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:502 / 512
页数:11
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