Vertical and horizontal heterogeneity of atmospheric dust loading in northern Gale Crater, Mars

被引:7
|
作者
Moore, Casey A. [1 ]
Moores, John E. [1 ]
Newman, Claire E. [2 ]
Lemmon, Mark T. [3 ]
Guzewich, Scott D. [4 ]
Battalio, Michael [3 ]
机构
[1] York Univ, CRESS, 4700 Keele St, Toronto, ON M3J 1P3, Canada
[2] Aeolis Res, Pasadena, CA 91107 USA
[3] Texas A&M Univ, Dept Atmospher Sci, MS 3150, College Stn, TX 77843 USA
[4] NASA Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
关键词
Mars; Atmospheric dust; Extinction; Opacity; Sedimentation; WATER-ICE CLOUDS; OPTICAL DEPTH; MARTIAN ATMOSPHERE; SEDIMENTARY-ROCKS; BOUNDARY-LAYER; LANDING SITE; ROVER; MSL; IMAGER; AEROSOL;
D O I
10.1016/j.icarus.2019.03.041
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
This paper updates the record of atmospheric dust loading within northern Gale Crater, Mars, by providing line of-sight extinction (LOS-Ext) measurements of the intervening dust between the rover and the crater rim. These measurements are derived from images taken with the Navigation Cameras (Navcam) onboard the Mars Science Laboratory (MSL) rover, Curiosity. The observations span 2.44 Mars years, from Mars Year (MY) 31 at a solar longitude (L-s) of 208 degrees to t L-s = 7 degrees of MY34, sols 100-1701 of the MSL surface mission. This work examines the dataset for seasonal trends of the LOS-Ext in addition to horizontal variations and the vertical structure of LOS-Ext. The LOS-Ext has a repetitive pattern with a single peak in the latter half of the Mars year. The atmosphere in the crater is well mixed horizontally but not vertically as larger LOS-Ext is seen nearer the crater floor than at higher altitudes within the crater. The results allow a discussion on whether or not Gale Crater is a sink for atmospheric dust or a source of atmospheric dust in the current era.
引用
收藏
页码:197 / 206
页数:10
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