通过OMEGA/Mars Express观测的火星北极帽的夏季演变
Y Langevin1, F Poulet, J-P Bibring
1Institut d'Astrophysique Spatiale, CNRS-Université Paris Sud, 91405 Orsay, France. yves.langevin@ias.u-psud.fr
概括
矿物质,水,冰和活动观测台 (OMEGA) 仪器监测了火星的水冰,观察了从小粒度到大粒度冰的转变. 在观察期间,表面冰的尘埃污染在最低水平.
科学领域:
- 行星科学 行星科学
- 天文地质学 天文地质学
- 遥感 遥感 遥感 遥感
背景情况:
- 火星的极地盖表现出水冰的范围和特性季节性变化.
- 了解表面冰的动态对于解释火星气候历史至关重要.
研究的目的:
- 为了监测火星北极地区的水冰和冰粒大小的时间演变.
- 评估表面冰的白色变化和尘埃污染.
主要方法:
- 使用OMEGA可见红外成像光谱仪进行广泛的观测.
- 在2004年底 (Ls 93-127度) 分析了来自火星北度 (北70度以上) 的数据.
- 随着时间的推移,监测了表面水冰的范围,颗粒大小和白色.
主要成果:
- 在极地帽上观察到从明亮的,小粒度的冰转变为较大粒度的冰.
- 观察到偏远地区的白度增加,这些地区以大粒度冰为主.
- 取决于模型的评估表明冰块的尘埃污染程度较低.
结论:
- 火星的北极帽季节性地经历着和冰粒属性的显著变化.
- 阿尔贝多变化与冰粒大小和分布的变化有关.
- 火星表面的水冰在此期间显示出有限的尘埃污染.
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