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首页> 外文期刊>Icarus: International Journal of Solar System Studies >Gale surface wind characterization based on the Mars Science Laboratory REMS dataset. Part I: Wind retrieval and Gale's wind speeds and directions
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Gale surface wind characterization based on the Mars Science Laboratory REMS dataset. Part I: Wind retrieval and Gale's wind speeds and directions

机译:基于火星科学实验室REMS数据集的大孔表面风力特征。 第一部分:风检索和大风的风速和方向

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The characterization of Martian surface winds as a function of time of day and season at one location can increase our knowledge of Mars surface conditions and assist in planning for future unmanned and manned missions. Martian surface winds vary greatly with location, and even at a particular landing site show a high degree of diurnal, seasonal, and interannual variability. Thus characterizing surface wind speeds and directions requires a long time series, which is rarely obtained on Mars. The Rover Environmental Monitoring Station (REMS) instrument on the Mars Science Laboratory (MSL) rover has been measuring Martian winds since 2012, thus has provided more than two Martian years of wind data at the first Martian landing site to have significant topography, in the trench of Gale Crater. Unfortunately, likely debris impacts during landing damaged the wind sensor, making it difficult to extract useful wind data. The first part of this paper presents a new retrieval that allows "good" wind measurements to be extracted from the raw dataset obtained under such conditions. In addition, a characterization of wind speeds and directions in Gale Crater is presented, after processing the full dataset of wind data in order to obtain the representative winds for different diurnal timeslots and seasons. Results suggest complex wind patterns and great variability depending on local time and season. Also, a significant influence by the synoptic scale circulation in the wind patterns is observed, although the local-scale circulation is suggested to be the major contributor to the observed surface winds in Gale Crater.
机译:Martian Surface Winds的表征​​在一个地点的一天和季节的功能可以增加我们对火星表面条件的了解,并协助规划未来无人驾驶和载人任务。火星表面风随着位置而异,甚至在特定的着陆场地均显示出高度的昼夜昼夜季节性和际变化。因此,表面风速和方向表征需要长时间序列,这很少在火星上获得。火星科学实验室(MSL)Rover的流浪者环境监测站(REMS)仪器自2012年以来一直在衡量火星风,因此在第一个火星着陆网站提供了两个以上的火星多年的风数据,以具有重要的地形,在大风陨石坑的沟渠。不幸的是,可能在着陆过程中堵塞损坏风传感器,使得难以提取有用的风数据。本文的第一部分呈现了一种新的检索,允许从在这种条件下获得的原始数据集中提取“良好”的风测量。此外,在处理风数据的完整数据集之后,提出了在大姿势喷气口中的风速和方向的表征,以便获得不同的昼夜时隙和季节的代表风。结果提出了复杂的风图案和巨大的变化,具体取决于当地时间和季节。而且,观察到风图案中的天气缩放循环的显着影响,尽管局部规模的循环被建议是大脑陨石坑中观察到的表面风的主要贡献者。

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