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Modeling Effects of Stellar UV-Driven Photochemistry on the Transit Spectra of Moist Rocky Atmospheres Around M Dwarfs

机译:恒星UV驱动光化学对M矮人潮湿岩石环境过境谱的建模效果

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3-D climate modeling has shown that tidally-locked terrestrial planets, at the inner habitable zone edge (IHZ) of M dwarf stars with T_(eff) > 3000 K, are able to retain a "moist" atmosphere (i.e. a water vapor rich stratosphere). However, flaring M dwarfs have strong UV activity, which may photodissociate this H_2O. Here, we employ a 1-D photochemical model with varied stellar UV, to assess whether H_2O loss driven by high stellar UV would affect H_2O detectability in JWST transmission spectroscopy. Temperature and water vapor profiles are taken from published 3-D climate model simulations of an IHZ Earth-sized planet around a 3300 K M dwarf with an N_2-H_2O atmosphere; they serve as self-consistent inputs for the 1-D model. We explore additional chemical complexity within the 1-D model by introducing other atmospheric species. In this paper, we review our methodology, focusing on the 1-D photochemical model.
机译:3-D气候建模表明,具有T_(EFF)> 3000 k的M个矮星恒星的内部可居住区域边缘(IHz)的各个锁定的地面行星能够保留“潮湿”的气氛(即水蒸气丰富的平流层)。然而,喇叭异性的m矮子具有强紫外线活性,这可能是光区分离该H_2O的。在这里,我们采用具有变化的恒星UV的1-D光学化学模型,以评估由高恒星UV驱动的H_2O损耗是否会影响JWST传输光谱中的H_2O可检测性。温度和水蒸气剖面来自发布的3-D气候模型模拟IHZ地球大小的行星,围绕3300 k M矮小的全球,具有N_2-H_2O气氛;它们作为1-D模型作为自我一致的输入。我们通过引入其他大气层来探讨1-D型号内的额外化学复杂性。在本文中,我们审查了我们的方法,专注于1-D光化学模型。

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