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Cloud features and zonal wind measurements of Saturn's atmosphere as observed by Cassini/VIMS

机译:卡西尼号/ VIMS观测到的土星大气云特征和纬向风测量

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We present an analysis of data about Saturn's atmosphere from Cassini's Visual and Infrared Mapping Spectrometer (VIMS), focusing on the meteorology of the features seen in the 5 μm spectral window. We present VIMS mosaics and discuss the morphology and general characteristics of the features backlit by Saturn's thermal emission. We have also constructed a zonal wind profile from VIMS feature tracking observation sequences using an automated cloud feature tracker. Comparison with previously constructed profiles from Voyager and Cassini imaging data reveals broad similarities, suggesting minimal vertical shear of the zonal wind. However, areas of apparent wind shear are present in the VIMS zonal wind profile at jet stream cores. In particular, our analysis shows that the equatorial jet reaches speeds exceeding 450 ms~(-1), similar to speeds obtained during the Voyager era. This suggests that recent inferences of relatively slower jet speeds of ~275-375 m s~(-1)are confined to the upper troposphere and that the deep (>1 bar) jet has not experienced a significant slowdown. Our measurements of the numerous dark, spotted features seen in the VIMS mosaics reveals that most of these features have diameters lessthan 1000 km and reside in confined zonal bands between jet stream cores. We propose that these spot features are vortices and that VIMS and Imaging Science Subsystem are sensing the same vortices at two different pressure levels. The local structure at the zonal jet streams remains complex, as VIMS may be sensing cloud features that are deeper than the NH_3 cloud deck.
机译:我们通过卡西尼号的视觉和红外映射光谱仪(VIMS)对有关土星大气的数据进行了分析,重点是在5μm光谱窗口中观测到的特征的气象学。我们介绍了VIMS马赛克,并讨论了土星热辐射背光特征的形态和一般特征。我们还使用自动云特征跟踪器根据VIMS特征跟踪观测序列构造了纬向风廓线。与Voyager和Cassini影像数据中先前构造的剖面的比较显示出广泛的相似性,表明纬向风的垂直切变最小。但是,在射流核心处的VIMS纬向风剖面中存在明显的风切变区域。特别是,我们的分析表明,赤道射流的速度超过了450 ms〜(-1),与航海家时代获得的速度相似。这表明最近的推论是相对较慢的射流速度〜275-375 m s〜(-1)仅限于对流层上部,而深层(> 1 bar)的射流并未经历明显的减速。我们对VIMS马赛克中看到的众多深色斑点特征的测量结果表明,这些特征大多数直径小于1000 km,并且位于射流流芯之间的封闭带状区域中。我们认为这些斑点特征是涡旋,而VIMS和影像科学子系统正在两个不同的压力水平下感应相同的涡旋。由于VIMS可能正在感测比NH_3云层更深的云特征,因此纬向射流的局部结构仍然很复杂。

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