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arXiv 1409.0519astro-ph.EP
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热木星大气中的磁效应

Magnetic Effects in Hot Jupiter Atmospheres

Tamara M. Rogers, Thaddeus D. Komacek

摘要:

本文对温度范围为1100- 1800 K的高温超导体大气进行了磁流体动力学(MHD)模拟。在温度为$\lesssim$ 1400 K的大气中,磁效应可以忽略不计。在较高的温度下,风是可变的,在许多情况下,平均赤道气流可能会向西,与它们的流体动力学对应物相反。欧姆耗散在温度$\sim$ 1500- 1600 K时达到峰值,取决于场强,最大值$\sim 10^{18}$ W在10 bar,大大低于先前的估计。根据所做的有限参数研究,该值不能随着风力增加、温度升高、场强升高、边界条件不同或扩散率降低而显著增加。虽然在这些模拟中没有解决,但有适度的证据表明,磁浮力不稳定性可能在热大气中进行。

英文摘要:

We present magnetohydrodynamic (MHD) simulations of the atmospheres of hot Jupiters ranging in temperature from 1100-1800K. Magnetic effects are negligible in atmospheres with temperatures $\lesssim$ 1400K. At higher temperatures winds are variable and in many cases, mean equatorial flows can become westward, opposite to their hydrodynamic counterparts. Ohmic dissipation peaks at temperatures $\sim$1500-1600K, depending on field strength, with maximum values $\sim 10^{18}$W at 10bar, substantially lower than previous estimates. Based on the limited parameter study done, this value can not be increased substantially with increasing winds, higher temperatures, higher field strengths, different boundary conditions or lower diffusivities. Although not resolved in these simulations there is modest evidence that a magnetic buoyancy instability may proceed in hot atmospheres.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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