Theory of Figures to the Seventh Order and the Interiors of Jupiter and Saturn

被引:46
作者
Nettelmann, N. [1 ,2 ]
Movshovitz, N. [1 ]
Ni, D. [3 ]
Fortney, J. J. [1 ]
Galanti, E. [4 ]
Kaspi, Y. [4 ]
Helled, R. [5 ]
Mankovich, C. R. [6 ]
Bolton, S. [7 ]
机构
[1] Univ Calif Santa Cruz, Dept Astron & Astrophys, Santa Cruz, CA 95064 USA
[2] German Aerosp Ctr, Inst Planetary Res, D-12489 Berlin, Germany
[3] Macau Univ Sci & Technol, State Key Lab Lunar & Planetary Sci, Macau, Peoples R China
[4] Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-7610001 Rehovot, Israel
[5] Univ Zurich, Inst Computat Sci, Ctr Theoret Astrophys & Cosmol, CH-8057 Zurich, Switzerland
[6] Caltech, Div Geol & Planetary Sci, Mailcode 150-21, Pasadena, CA 91125 USA
[7] Southwest Res Inst, San Antonio, TX 78238 USA
来源
PLANETARY SCIENCE JOURNAL | 2021年 / 2卷 / 06期
关键词
Jupiter; Planetary interior; Saturn; HELIUM ABUNDANCE; ZONAL FLOWS; GRAVITY; ATMOSPHERE; CONSISTENT; EQUATION; HYDROGEN; MODELS; DEPTH;
D O I
10.3847/PSJ/ac390a
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Interior modeling of Jupiter and Saturn has advanced to a state where thousands of models are generated that cover the uncertainty space of many parameters. This approach demands a fast method of computing their gravity field and shape. Moreover, the Cassini mission at Saturn and the ongoing Juno mission delivered gravitational harmonics up to J (12). Here we report the expansion of the theory of figures, which is a fast method for gravity field and shape computation, to the seventh order (ToF7), which allows for computation of up to J (14). We apply three different codes to compare the accuracy using polytropic models. We apply ToF7 to Jupiter and Saturn interior models in conjunction with CMS-19 H/He equation of state. For Jupiter, we find that J (6) is best matched by a transition from an He-depleted to He-enriched envelope at 2-2.5 Mbar. However, the atmospheric metallicity reaches 1 x solar only if the adiabat is perturbed toward lower densities, or if the surface temperature is enhanced by similar to 14 K from the Galileo value. Our Saturn models imply a largely homogeneous-in-Z envelope at 1.5-4 x solar atop a small core. Perturbing the adiabat yields metallicity profiles with extended, heavy-element-enriched deep interior (diffuse core) out to 0.4 R (Sat), as for Jupiter. Classical models with compact, dilute, or no core are possible as long as the deep interior is enriched in heavy elements. Including a thermal wind fitted to the observed wind speeds, representative Jupiter and Saturn models are consistent with all observed J ( n ) values.
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页数:18
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