首页> 外文期刊>Icarus: International Journal of Solar System Studies >Composition and structure of fresh ammonia clouds on Jupiter based on quantitative analysis of Galileo/NIMS and New Horizons/LEISA spectra
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Composition and structure of fresh ammonia clouds on Jupiter based on quantitative analysis of Galileo/NIMS and New Horizons/LEISA spectra

机译:基于伽利略/尼姆的定量分析和新的地平线/巢穴光谱的木星上新鲜氨云的组成与结构

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Ammonia gas has long been assumed to be the main source of condensables for the upper cloud layer on Jupiter, but distinctive spectral features associated with ammonia have been seen only rarely. Since both ammonia and NH4SH absorb in the 3 mu m region, and widespread absorption in the 3 mu m region was present (Sromovsky and Fry, 2010), identification of the 2 mu m absorption feature of NH3 provided an opportunity to clearly establish its presence in Jovian clouds. Baines et al. (2002) succeeded in finding in Near Infrared Mapping Spectrometer (NIMS) observations one feature that had both 2 mu m and 3 mu m absorption, and many which were known to have absorption at 2.73 mu m. They named these Spectrally Identifiable Ammonia Clouds (SIACs). They also argued that these were fresh ammonia clouds that would eventually succumb to some process that would obscure their absorption features. Detection of many more of the 2 mu m features was later achieved by New Horizon's Linear Etalon Imaging Spectral Array (LEISA) instrument, which provided both the spatial and spectral resolution needed to identify these features. Here we report on the first quantitative modeling that uses NIMS spectra over a broad (1-5.2 mu m) spectral range and LEISA spectra over a much narrower (1.25-2.5 mu m) spectral range to constrain the cloud structure and composition of these rare cloud features and compare them to background clouds. We find that the absorption signature at 2 mu m, which is well characterized in LEISA spectra, is relatively subtle and easily matched by model clouds containing spherical particles of ammonia ice with radii of 2-4 mu m. The NIMS spectra, which cover both reflected sunlight as well as thermal emission regions are more difficult to model with cloud materials plausibly present in Jupiter's atmosphere. The best signal/noise spectra obtained from NIMS provide a relatively sparse sampling of the spectrum, which does not establish the detailed shape of the 3 mu m absorpti
机译:长期以来,氨气已经被认为是木星上云层的凝聚物的主要来源,但与氨相关的独特谱特征很少被人们看到。由于氨和NH4SH吸收3μm地区,并且在3亩地区的广泛吸收(Sromovsky和Fry,2010)中,NH3的2μm吸收特征的鉴定提供了明确建立其存在的机会在jovian云中。 Baines等人。 (2002)成功发现近红外线映射光谱仪(NIMS)观察均具有2μm和3μm吸收的一个特征,并且许多已知在2.73μm处具有吸收。他们将这些光谱识别的氨云(SIACS)命名。他们还认为,这些是新鲜的氨云,最终会屈服于一些会掩盖吸收特征的过程。通过新的Horizo​​ n的线性标准具成像谱阵列(LESISA)仪器稍后检测到2μm的许多特征,提供了识别这些特征所需的空间和光谱分辨率。在这里,我们报告了在较大(1.25-2.5μm)光谱范围内使用宽(1-5.2μm)光谱范围和巢穴光谱来限制这些稀有的云结构和组成的第一定量建模云特征并将它们与背景云进行比较。我们发现,在淡景光谱中,2 mu m的吸收签名是相对微妙的,并且通过含有2-4μm的半径的氨冰球颗粒的模型云容易地匹配。覆盖反射的阳光以及热发射区域的NIMS光谱更难以用云材料呈现在木星的大气中。从NIM获得的最佳信号/噪声光谱提供了光谱的相对稀疏的采样,其不建立3μm脱落剂的详细形状

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