土星夏至时的季节性大气
Saturn's Seasonal Atmosphere at Northern Summer Solstice
AI总结:
本研究基于卡西尼号任务数据,梳理土星北半球春分到夏至的大气季节变化,验证相关气候模型,指出模型与观测的差异及动力学的重要性,并展望未来土星季节探测的需求。
摘要:
卡西尼号土星轨道任务惊人的持续时长,为我们提供了迄今为止对一颗存在季节变化的巨行星最全面的探测。本综述探究了2015-2017年土星北半球春分到夏至期间全球温度、成分和气溶胶特性的变化,将我们此前关于卡西尼号遥感探测的综述(2004-2014年,Fletcher等人,2018年)拓展至任务的“壮丽终章”阶段。研究得到了一份前所未有的土星气候记录,时长跨度接近半个土星年,可用于检验辐射气候模型、中性与离子光化学模型以及大气环流模型的季节预测结果。研究观测到,对流层和平流层温度的半球不对称性从北半球冬季到北半球夏季发生反转;碳氢化合物和仲氢的空间分布随大气动力学过程(例如季节反转的哈得来环流、极地平流层涡旋形成、赤道平流层振荡以及半球间输送)发生变化;对流层上部和平流层气溶胶的光学厚度出现改变,调节了土星的可见颜色(夏至前后北半球从蓝色调变为金色外观)、反射率和近红外发射特性。辐射平衡与光化学的数值模拟能够很好地重现观测到的季节变化和相位滞后,但模型与观测结果之间仍存在差异,这表明大气动力学发挥着关键作用,且需要将化学与辐射方案耦合到下一代环流模型中。随着卡西尼号任务终结,对土星从北半球夏季到秋季的季节变化开展长期研究,将需要地基和天基天文台的探测能力,同时我们也热切期待下一颗土星轨道探测器的到来。
英文摘要:
The incredible longevity of Cassini's orbital mission at Saturn has provided the most comprehensive exploration of a seasonal giant planet to date. This review explores Saturn's changing global temperatures, composition, and aerosol properties between northern spring and summer solstice (2015-2017), extending our previous review of Cassini's remote sensing investigations (2004-14, Fletcher et al., 2018) to the grand finale. The result is an unprecedented record of Saturn's climate that spans almost half a Saturnian year, which can be used to test the seasonal predictions of radiative climate models, neutral and ion photochemistry models, and atmospheric circulation models. Hemispheric asymmetries in tropospheric and stratospheric temperatures were observed to reverse from northern winter to northern summer; spatial distributions of hydrocarbons and para-hydrogen shifted in response to atmospheric dynamics (e.g., seasonally-reversing Hadley cells, polar stratospheric vortex formation, equatorial stratospheric oscillations, and inter-hemispheric transport); and upper tropospheric and stratospheric aerosols exhibited changes in optical thickness that modulated Saturn's visible colours (from blue hues to a golden appearance in the north near solstice), reflectivity, and near-infrared emission. Numerical simulations of radiative balance and photochemistry do a good job in reproducing the observed seasonal change and phase lags, but discrepancies between models and observations still persist, indicating a crucial role for atmospheric dynamics and the need to couple chemical and radiative schemes to the next generation of circulation models. With Cassini's demise, an extended study of Saturn's seasons, from northern summer to autumn, will require the capabilities of ground- and space-based observatories, as we eagerly await the next orbital explorer at Saturn.
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