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Cloud formation in substellar atmospheres

机译:云形成在FOLLELLAR EMOTOSHERES

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Clouds seem like an every-day experience. But — do we know how clouds form on browndwarfs and extra-solar planets? How do they look like? Can we see them? What are they composedof? Cloud formation is an old-fashioned but still outstanding problem for the Earth atmosphere,and it has turned into a challenge for the modelling of brown dwarf and exo-planetary atmospheres.Cloud formation imposes strong feedbacks on the atmospheric structure, not only due to the cloudsown opacity, but also due to the depletion of the gas phase, possibly leaving behind a dynamicand still supersaturated atmosphere. I summarise the different approaches taken to model cloudformation in substellar atmospheres and workout their differences. Focusing on the phase-non-equilibrium approach to cloud formation, I demonstrate the inside we gain from detailed micro-physical modelling on for instance the material composition and grain size distribution inside thecloud layer on a Brown Dwarf atmosphere. A comparison study on four different cloud approachesin Brown Dwarf atmosphere simulations demonstrates possible uncertainties in interpretation ofobservational data.
机译:云看起来像一个每日使用体验。但是 - 我们知道云是如何形成的browndwarfs和外太阳系外行星?他们怎么样子?我们可以看到他们?它们是什么composedof?云的形成是地球大气层的老式,但依然突出问题,它已变成了褐矮星和外行星atmospheres.Cloud形成的造型是一个挑战强加给大气结构强烈反馈,不仅因cloudsown不透明,而且由于气相的枯竭,可能留下dynamicand仍然过饱和的气氛后面。我总结亚恒星大气和锻炼他们的分歧带到模型cloudformation不同的办法。着眼于相位非平衡的方法来云的形成,我展示从thecloud层内例如材料组成和粒度分布的详细微物理模型内我们获得上的布朗矮气氛。在四个不同的云approachesin褐矮星大气模拟的比较研究表明在解释ofobservational数据可能的不确定性。

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