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Numerical simulations on origin of Galilean moons' magnetic anomalies

Numerical simulations on origin of Galilean moons' magnetic anomalies

作     者:JIAO LiGuo KUANG WeiJia MA ShiZhuang 

作者机构:Laboratory of Computational Geodynamics College of Earth Sciences Graduate University of Chinese Academy of Sciences Beijing 100049 China NASA Goddard Space Flight Center Greenbelt MD 20771 USA 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2011年第54卷第12期

页      面:1754-1760页

核心收录:

学科分类:070801[理学-固体地球物理学] 06[历史学] 060207[历史学-专门史] 07[理学] 0708[理学-地球物理学] 0712[理学-科学技术史(分学科,可授理学、工学、农学、医学学位)] 0602[历史学-中国史] 

基  金:supported by National Natural Science Foundation of China (Grant No. 40328006) 

主  题:Galilean moons magnetic fields magneto-convection dynamo 

摘      要:Galileo mission detected the magnetic anomalies originated from Galilean *** anomalies are likely generated in the moons interiors,under the influence of a strong ambient Jovian *** various possible generation mechanisms of the anomalies,we focus on magneto-convection and dynamos in the interiors via numerical *** mimic the electromagnetic environment of the moons,we introduce in our numerical model an external uniform magnetic field B0 with a fixed orientation but varying field *** results show that a finite B0 can substantially alter the dynamo processes inside the *** the ambient field strength B0 increases to approximately 40% of the field generated by the pure dynamo action,the convective state in the core changes significantly:the convective flow decreases by 80% in magnitude,but the differential rotation becomes stronger in much of the fluid layer,leading to a stronger field generated in the *** field morphologies inside the core tend to align with the ambient field,while the flow patterns show the symmetry-breaking effect under the influence of ***,the generated field tends to be temporally more stable.

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