MAGNETOSPHERIC STRUCTURE AND ATMOSPHERIC JOULE HEATING OF HABITABLE PLANETS ORBITING M-DWARF STARS

被引:97
作者
Cohen, O. [1 ]
Drake, J. J. [1 ]
Glocer, A. [2 ]
Garraffo, C. [1 ]
Poppenhaeger, K. [1 ]
Bell, J. M. [3 ]
Ridley, A. J. [4 ]
Gombosi, T. I. [4 ]
机构
[1] Harvard Smithsonian Ctr Astrophys, Cambridge, MA 02138 USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] Natl Inst Aerosp, Ctr Planetary Atmospheres & Flight Sci, Hampton, VA 23666 USA
[4] Univ Michigan, Ctr Space Environm Modeling, Ann Arbor, MI 48109 USA
关键词
magnetohydrodynamics ( MHD); planets and satellites: atmospheres; planets and satellites: magnetic fields; planets and satellites: terrestrial planets; RESISTIVE MHD SIMULATIONS; EARTH-LIKE EXOPLANETS; EJECTION CME ACTIVITY; MASS-LOSS RATES; X-RAY-EMISSION; MAGNETIC-FIELD; HOT JUPITERS; GANYMEDES MAGNETOSPHERE; TERRESTRIAL EXOPLANETS; CIRCULATION MODELS;
D O I
10.1088/0004-637X/790/1/57
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We study the magnetospheric structure and the ionospheric Joule Heating of planets orbiting M-dwarf stars in the habitable zone using a set ofmagnetohydrodynamic models. The stellarwind solution is used to drive amodel for the planetary magnetosphere, which is coupled with a model for the planetary ionosphere. Our simulations reveal that the space environment around close-in habitable planets is extreme, and the stellar wind plasma conditions change from sub-to super-Alfv ' enic along the planetary orbit. As a result, themagnetospheric structure changes dramatically with a bow shock forming in the super-Alfv ' enic sectors, while no bow shock forms in the sub-Alfv ' enic sectors. The planets reside most of the time in the sub-Alfv ' enic sectors with poor atmospheric protection. A significant amount of Joule Heating is provided at the top of the atmosphere as a result of the intense stellar wind. For the steady-state solution, the heating is about 0.1%-3% of the total incoming stellar irradiation, and it is enhanced by 50% for the time-dependent case. The significant Joule Heating obtained here should be considered in models for the atmospheres of habitable planets in terms of the thickness of the atmosphere, the top-side temperature and density, the boundary conditions for the atmospheric pressure, and particle radiation and transport. Here we assume constant ionospheric Pedersen conductance similar to that of the Earth. The conductance could be greater due to the intense EUV radiation leading to smaller heating rates. We plan to quantify the ionospheric conductance in future study.
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页数:13
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