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首页> 外文期刊>Icarus: International Journal of Solar System Studies >Saturn's upper atmosphere during the Voyager era: Reanalysis and modeling of the UVS occultations
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Saturn's upper atmosphere during the Voyager era: Reanalysis and modeling of the UVS occultations

机译:航海家时代的土星高空大气:UVS掩星的重新分析和建模

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The Voyager 1 and 2 Ultraviolet Spectrometer (UVS) solar and stellar occultation dataset represents one of the primary, pre-Cassini sources of information that we have on the neutral upper atmosphere of Saturn. Despite its importance, however, the full set of occultations has never received a consistent, nor complete, analysis, and the results derived from the initial analyses over thirty years ago left questions about the temperature and density profiles unanswered. We have reanalyzed all six of the UVS occultations (three solar and three stellar) to provide an up-to-date, pre-Cassini view of Saturn's upper atmosphere. From the Voyager UVS data, we have determined vertical profiles for H-2, H, CH4, C2H2, C2H4, and C2H6, as well as temperature. Our analysis also provides explanations for the two different thermospheric temperatures derived in earlier analyses (400-450 K versus 800 K) and for the unusual shape of the total density profile noted by Hubbard et al. (1997). Aside from inverting the occultation data to retrieve densities and temperatures, we have investigated the atmospheric structure through a series of photochemical models to infer the strength of atmospheric mixing and other physical and chemical properties of Saturn's mesopause region during the Voyager flybys. We find that the data exhibit considerable variability in the vertical profiles for methane, suggesting variations in vertical winds or the eddy diffusion coefficient as a function of latitude and/or time in Saturn's upper atmosphere. The results of our reanalysis will provide a useful baseline for interpreting new data from Cassini, particularly in the context of change over the past three decades. (C) 2015 Elsevier Inc. All rights reserved.
机译:Voyager 1和2型紫外线光谱仪(UVS)的太阳和恒星掩星数据集代表了我们在土星中性高层大气中拥有的卡西尼前信息的主要来源之一。尽管它的重要性,但是整个掩星掩盖术从未得到一致,完整的分析,而三十多年前的初步分析结果却未回答有关温度和密度分布的问题。我们重新分析了UVS的所有六种掩星(三个太阳星和三个恒星),以提供卡西尼号之前土星高层大气的最新视图。根据Voyager UVS数据,我们确定了H-2,H,CH4,C2H2,C2H4和C2H6的垂直剖面以及温度。我们的分析还为较早的分析中得出的两种不同的热层温度(400-450 K与800 K)以及Hubbard等人指出的总密度分布的不寻常形状提供了解释。 (1997)。除了颠倒掩星数据以获取密度和温度以外,我们还通过一系列光化学模型研究了大气结构,以推断旅行者号飞越期间土星的更年期区域的大气混合强度和其他理化特性。我们发现,这些数据在甲烷的垂直剖面上显示出相当大的可变性,表明垂直风或涡流扩散系数的变化是土星高层大气中纬度和/或时间的函数。我们的重新分析结果将为解释卡西尼号的新数据提供有用的基线,尤其是在过去三十年的变化情况下。 (C)2015 Elsevier Inc.保留所有权利。

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