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首页> 外文期刊>Icarus: International Journal of Solar System Studies >Sporadic formation of slope streaks on Mars
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Sporadic formation of slope streaks on Mars

机译:火星上斜坡条纹的零星形成

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Slope streaks are a form of gravity-driven mass-movements that frequently occur on Mars today. The cause of slope streak formation remains unclear; both, dry and wet processes have been suggested. Here, we observationally constrain the time of the year during which slope streaks form. Imagery from four Mars-orbiting cameras is mined to identify locations that have been imaged repeatedly, and the overlapping images are surveyed for streak activity. A search algorithm automatically finds the locations on the surface that have been imaged most often based on a graph representation. Dark slope streaks are found to form sporadically throughout the Mars year. At one study site in the Olympus Mons Aureole, observations constrain slope streak formation to at least five distinct time intervals within a single Mars year. New slope streaks form spatially isolated or in small groups within a few kilometers of one another. The observations suggest that slope streak triggering is unrelated to season and not caused by any large regional events. Most slope streaks are caused by sporadic events of small spatial extent.
机译:倾斜条纹是当今火星上经常发生的重力驱动的质量运动形式。斜坡条纹形成的原因尚不清楚;已经提出了干法和湿法两种方法。在这里,我们观察地限制一年中形成斜条纹的时间。挖掘来自四个火星轨道摄像机的图像,以识别已重复成像的位置,并调查重叠图像的条纹活动。搜索算法会根据图形表示自动找到最常成像的表面位置。在整个火星年,发现零星地形成了黑边条纹。在奥林匹斯山(Olympus Mons Aureole)的一个研究地点,观察将斜坡条纹的形成限制在单个火星年内至少五个不同的时间间隔。新的斜坡条纹在空间上相互隔离,或者彼此之间相距仅几千米。观测结果表明,斜坡条纹触发与季节无关,也不是由任何大型区域性事件引起的。大多数斜坡条纹是由空间范围较小的零星事件引起的。

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