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26 April 2024
 
  » arxiv » 1101.0691

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The role of rotation on the evolution of dynamo generated magnetic fields in Super Earths
Jorge I. Zuluaga ; Pablo A. Cuartas-Restrepo ;
Date 4 Jan 2011
AbstractPlanetary magnetic fields could have a role on the evolution of planetary atmospheres and the required conditions for the emergence and evolution of life (habitability). After briefly review the current efforts to study the evolution of dynamo generated magnetic fields in massive earth-like rocky planets (Super Earths), we take the results from thermal evolution models and updated scaling laws for convection driven magnetodynamos to predict the evolution of the local Rossby number, the basic indicator of core magnetic field geometry and regime. We study the dependence of this property on planetary mass and rotation rate. Previous works have paid Attention only to the evolution of dipolar dominant core magnetic fields assuming rapid rotating planets. Here we extend these results including consistently the effects of rotation on the evolution of planetary magnetic field properties and obtain global constraints to the existence of intense protective magnetic fields in rapidly and slowly rotating Super Earths. We find that the emergence and endurance of a protective planetary magnetic field would not be only a function of planetary mass but also would depend on rotation rates in interesting ways. Low mass Super Earths ($M<2ME$) would develop an intense surface magnetic field but its lifetime will be limited to 2-4 Gyrs for rotational periods exceeding 1.5 days. On the other hand and also in the case of slowly rotating planets more massive Super Earths will have a weak magnetic fields but their dipoles would last longer. Finally we analyze the case for tidally locked Super Earths inside and outside the habitable zone of GKM stars where long rotation periods will be common. Using the results obtained here we develop a classification of Super Earths based on their rotation and depending on the emergent evolving properties of dynamo generated planetary magnetic fields.
Source arXiv, 1101.0691
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