Thermal Impacts of Atmospheric Gravity Waves in the Martian Thermosphere

IF 3.9 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Scott L. England, Aishwarya Kumar, Guiping Liu, Mehdi Benna
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Abstract

Observations of the Martian thermosphere have revealed small-scale, large amplitude fluctuations believed to be associated with atmospheric gravity waves (GWs). Previous analysis of the MAVEN Neutral Gas and Ion Mass Spectrometer (NGIMS) data has described the overall behavior of these waves and their consistency with GW theory. One of the key impacts of these waves as they dissipate is the heating and cooling of the neutral atmosphere, from both deposition of the energy and transporting heat. While initial evidence for this has been presented, systematic patterns in heating and cooling require the analysis of a long-term data set. This study examines 5 years of NGIMS data to systematically determine the thermal impact of GWs in the thermosphere, and variations with location, season and local time. While both viscous heating and cooling from sensible heat flux are significant at the altitudes seen with NGIMS, cooling tends to dominate in the cases examined. Clear variations in the heating and cooling are seen with the background atmospheric density, with a large degree of variability in addition to this, reflecting the high degree of variations in GWs seen in the thermosphere. Seasonal variations in the net thermal impact of GWs are apparent at mid-high latitudes, and less clear near the equator. During times when MAVEN's periapsis is deeper inside the atmosphere, clear increases in the net thermal impact of GWs with altitude are evident. The overall results are consistent with some prior simulations but include altitudes and conditions not reported in those studies.

火星热层中大气重力波的热影响
对火星热层的观测揭示了据信与大气重力波(GWs)有关的小尺度、大幅度波动。先前对MAVEN中性气体和离子质谱仪(NGIMS)数据的分析已经描述了这些波的总体行为及其与GW理论的一致性。这些波消散的关键影响之一是中性大气的加热和冷却,这是由能量的沉积和热量的传递造成的。虽然已经提出了这方面的初步证据,但加热和冷却方面的系统模式需要对一组长期数据进行分析。本研究分析了5年的NGIMS数据,以系统地确定热层中GWs的热影响,以及随地点、季节和当地时间的变化。虽然在NGIMS观测到的高度,来自感热通量的粘性加热和冷却都很重要,但在所检查的情况下,冷却往往占主导地位。在背景大气密度中可以看到加热和冷却的明显变化,除此之外还有很大程度的变率,反映了在热层中看到的GWs的高度变化。GWs净热影响的季节变化在中高纬度地区很明显,在赤道附近不太明显。当MAVEN的近日点在大气层深处时,GWs的净热影响随着高度的增加而明显增加。总体结果与先前的一些模拟一致,但包括了那些研究中未报告的海拔和条件。
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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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