JpGU-AGU Joint Meeting 2017

講演情報

[JJ] ポスター発表

セッション記号 M (領域外・複数領域) » M-GI 地球科学一般・情報地球科学

[M-GI32] [JJ] 計算科学による惑星形成・進化・環境変動研究の新展開

2017年5月22日(月) 15:30 〜 17:00 ポスター会場 (国際展示場 7ホール)

コンビーナ:林 祥介(神戸大学・大学院理学研究科 惑星学専攻/惑星科学研究センター(CPS))、小河 正基(東京大学大学院総合文化研究科広域科学専攻)、井田 茂(東京工業大学大学院理工学研究科地球惑星科学専攻)、草野 完也(名古屋大学宇宙地球環境研究所)

[MGI32-P03] 回転球殻内の非弾性熱対流の臨界モードに対する熱拡散係数の動径分布の影響

*佐々木 洋平1竹広 真一3石渡 正樹2山田 道夫3 (1.京都大学大学院理学研究科数学教室、2.北海道大学大学院理学院宇宙理学専攻、3.京都大学数理解析研究所)

キーワード:臨界対流、非弾性流体、木星型惑星

Linear stability analysis of anelasitc thermal convection in a rotating spherical shell with thermal diffusivities varying in the radial direction is performed. The structures of critical convection are obtained in the cases of four different radial distributions of thermal diffusivity; (1) κ is constant, (2) κT0 is constant, (3) κρ0 is constant, and (4) κρ0T0 is constant, where κ is the thermal diffusivity, T0 is the temperature of basic state, and ρ0 is the density of basic state, respectively. The ratio of inner and outer radii, the Prandtl number, the polytrope index, and the density ratio are 0.35, 1, 2, and 5, respectively. The value of the Ekman number is 10-3 or 10-5 . In the case of (1), where the setup is same as that of the anelastic dynamo benchmark (Jones et al., 2011), the structure of critical convection is concentrated near the outer boundary of the spherical shell around the equator. However, in the cases of (2), (3) and (4), the convection columns attach the inner boundary of the spherical shell.

A rapidly rotating annuls model for anelastic systems is developed by assuming that convection structure is uniform in the axial direction taking into account the strong effect of Coriolis force. The annulus model well explains the characteristics of critical convection obtained numerically, such as critical azimuthal wavenumber, frequency, Rayleigh number, and the cylindrically radial location of convection coulumns.

The radial distribution of thermal diffusivity is important for convection structure, because it determines the distribution of radial basic entropy gradient which is crucial for location of convection columns.