日本地球惑星科学連合2019年大会

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[E] 口頭発表

セッション記号 P (宇宙惑星科学) » P-PS 惑星科学

[P-PS05] Recent advances of Venus science

2019年5月27日(月) 09:00 〜 10:30 A03 (東京ベイ幕張ホール)

コンビーナ:佐藤 毅彦(宇宙航空研究開発機構・宇宙科学研究本部)、堀之内 武(北海道大学地球環境科学研究院)、山本 勝(九州大学応用力学研究所)、Kevin McGouldrick(University of Colorado Boulder)、座長:Takeshi Horinouchi

09:00 〜 09:15

[PPS05-01] Super-rotation of Venusian atmosphere in the equatorial region may be caused by the density driven separation

*Adhithiyan Neduncheran1Ugur Guven1,2Ananyo Bhattacharya3 (1.University of Petroleum and Energy Studies, India、2.United Nations Centre for Space Science and Technology Education in Asia and the Pacific、3.Sardar Vallabhbhai National Institute of Technology,India)

キーワード:Venus, atmosphere, super-rotation, clouds, flow simulation

On Venus, the clouds move nearly 60 times faster than the rotation of the planet. Super-rotation of the Venusian atmosphere is an intriguing phenomena and the reasons are still unclear. The super-rotation is possibly due to Venus being tidally locked to Sun as a consequence of which the planet experiences maximum heating in the equatorial zones causing meridional flows in the lower latitudes. The latent heat trapped by the Carbon dioxide gradually rises above due to its increased kinetic energy, which increases the motion of the cloud layers over time. Previous works done shows that the clouds are highly unstable in the altitude ranging from 49-55Km and below 30Km as per Zasova et al 2006 (doi:10.1016/j.pss.2007.01.011 ). This work shall put forth a possibility of density driven separation of cloud layers and its viscosity which helps in the super-rotation of the clouds. Similar hypothesis were presented by Lebonnois et al 2017 (DOI: 10.1038/NGEO2971). Using the known densities of atmospheric constituents, and applying the principles of viscosity and fluid dynamics, a simulation in COMSOL Multiphysics is done and analyzed for the flow behavior in the atmospheric layers ranging between 20Km and 80Km with respect to it’s horizontal distance. The possible reasons regarding the flow will be discussed considering the solar convection in the equatorial region.