ExoMars TGO上NOMAD UVIS观测的火星气溶胶气候学

IF 3.9 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Z. Flimon, J. Erwin, S. Robert, L. Neary, A. Piccialli, L. Trompet, Y. Willame, F. Vanhellemont, F. Daerden, S. Bauduin, M. Wolff, I. R. Thomas, B. Ristic, J. P. Mason, C. Depiesse, M. R. Patel, G. Bellucci, J.-J. Lopez-Moreno, A. C. Vandaele
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引用次数: 0

摘要

2018年4月,痕量气体轨道器上的“火星发现”光谱仪开始科学运行,提供火星大气的红外和紫外可见光谱。本文探讨了UVIS通道在太阳掩星研究气溶胶中的应用。我们已经开发了一个检索方案,使我们能够研究气溶胶的大小和消失作为高度的函数。报告并讨论了从34岁中期到36岁末期的结果。采用对数正态分布的Mie码,有效半径(reff)为0.1 ~ 0.8 μm,有效方差(veff)为0.1。在这项工作中,我们展示了气溶胶分离层的存在,其特征是颗粒大小的局部增加和消失。这些分离层可以由灰尘、水冰或二氧化碳冰组成。CO2冰云可以在80千米的高空被探测到,而H2O冰云通常在30-50千米的高空被探测到。观察到粒子有效半径在南北区域之间的对称性。在南北冬季,大气气溶胶主要由0.6 μm以下的小颗粒组成,而在夏季,气溶胶的大小增加到微米级,超过了紫外可见光谱的灵敏度。这种在北部/南部夏季的规模增加与类似的灭绝增加无关。我们的数据支持先前观测到的水汽和气溶胶之间的关系,特别是在全球沙尘暴事件期间高空水冰云的形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Aerosol Climatology on Mars as Observed by NOMAD UVIS on ExoMars TGO

Aerosol Climatology on Mars as Observed by NOMAD UVIS on ExoMars TGO

The Nadir and Occultation for MArs Discovery spectrometer on board Trace Gas Orbiter began science operations in April 2018, providing infrared and ultraviolet-visible spectra of the Martian atmosphere. This paper explores the application of the UVIS channel in solar occultation to study aerosols. We have developed a retrieval scheme that allows us to study the size and extinction of the aerosol as a function of altitude. Results from mid-MY 34 to the end of MY 36 are reported and discussed. Particle size is retrieved using a Mie code with log-normal distribution with an effective radius (reff), 0.1–0.8 μm and an effective variance (veff) equal 0.1. In this work, we show the presence of aerosol-detached layers, characterized by a local increase in particle size and extinction. These detached layers can be composed of dust, H2O ice, or CO2 ice. CO2 ice clouds can be detected up to 80 km, while H2O ice clouds are usually more present around 30–50 km. Symmetry of the particle effective radius between the northern and southern regions is observed. During northern/southern winter, the atmospheric aerosols are composed of smaller particles below 0.6 μm but in summer, the size increases to micron-sized particles that are larger than the sensitivity of UVIS. This increase in size in the northern/southern summer is not correlated with a similar increase in extinction. Our data support the previously observed relationship between water vapor and aerosol, especially the formation of high-altitude water ice cloud during the global dust storm event.

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来源期刊
Journal of Geophysical Research: Planets
Journal of Geophysical Research: Planets Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
8.00
自引率
27.10%
发文量
254
期刊介绍: The Journal of Geophysical Research Planets is dedicated to the publication of new and original research in the broad field of planetary science. Manuscripts concerning planetary geology, geophysics, geochemistry, atmospheres, and dynamics are appropriate for the journal when they increase knowledge about the processes that affect Solar System objects. Manuscripts concerning other planetary systems, exoplanets or Earth are welcome when presented in a comparative planetology perspective. Studies in the field of astrobiology will be considered when they have immediate consequences for the interpretation of planetary data. JGR: Planets does not publish manuscripts that deal with future missions and instrumentation, nor those that are primarily of an engineering interest. Instrument, calibration or data processing papers may be appropriate for the journal, but only when accompanied by scientific analysis and interpretation that increases understanding of the studied object. A manuscript that describes a new method or technique would be acceptable for JGR: Planets if it contained new and relevant scientific results obtained using the method. Review articles are generally not appropriate for JGR: Planets, but they may be considered if they form an integral part of a special issue.
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