2012
DOI: 10.1088/0004-637x/750/1/74
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NEW H2COLLISION-INDUCED ABSORPTION AND NH3OPACITY AND THE SPECTRA OF THE COOLEST BROWN DWARFS

Abstract: We present new cloudy and cloudless model atmospheres for brown dwarfs using recent ab initio calculations of the line list of ammonia (NH 3 ) and of the collision-induced absorption of molecular hydrogen (H 2 ). We compare the new synthetic spectra with models based on an earlier description of the H 2 and NH 3 opacities. We find a significant improvement in fitting the nearly complete

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Cited by 121 publications
(186 citation statements)
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“…The spectrum of GJ 758 B is not well-matched by other empirical data of similar objects, specifically T6-T8 SpeX Prism standards, especially in the H band peak near 1.58 μm. K c data at 2.1 μm does not seem to be a discriminator for spectral type, but such longer wavelength data (including L′ and Ms, Janson et al 2011, not shown in figure) will be important in establishing g log , T eff , [Fe/H], and cloud cover from current (e.g., Morley et al 2012;Saumon et al 2012;Allard 2014) and future improved atmospheric models.…”
Section: Model Atmospheresmentioning
confidence: 99%
“…The spectrum of GJ 758 B is not well-matched by other empirical data of similar objects, specifically T6-T8 SpeX Prism standards, especially in the H band peak near 1.58 μm. K c data at 2.1 μm does not seem to be a discriminator for spectral type, but such longer wavelength data (including L′ and Ms, Janson et al 2011, not shown in figure) will be important in establishing g log , T eff , [Fe/H], and cloud cover from current (e.g., Morley et al 2012;Saumon et al 2012;Allard 2014) and future improved atmospheric models.…”
Section: Model Atmospheresmentioning
confidence: 99%
“…FeH), weak or absent metal oxides (e.g. VO and CO), and enhanced collision-induced H2 absorption (CIA H2;Bates 1952;Borysow, Frommhold, & Moraldi 1989;Borysow, Jorgensen, & Fu 2001;Abel et al 2012;Saumon et al 2012) in the nearinfrared (NIR).…”
mentioning
confidence: 99%
“…Those data were used to place the object in a diagram of M W 2 versus J − W 2, where W 2 is a band from the Widefield Infrared Survey Explorer (Wright et al 2010) that is similar to [4.5] from Spitzer. The position of WISE 0855-0714 in that diagram was better reproduced by cloudy models than cloudless models (Morley et al 2012(Morley et al , 2014aSaumon et al 2012), which was interpreted as evidence of water ice clouds. However, Luhman & Esplin (2014) demonstrated that WISE 0855-0714 was roughly midway between those cloudless and cloudy models in a similar diagram of M 4.5 versus J −[4.5], and that its position was best matched by cloudless models that employed nonequilibrium chemistry (Saumon & Marley 2008;Saumon et al 2012).…”
Section: Discussionmentioning
confidence: 91%
“…The position of WISE 0855-0714 in that diagram was better reproduced by cloudy models than cloudless models (Morley et al 2012(Morley et al , 2014aSaumon et al 2012), which was interpreted as evidence of water ice clouds. However, Luhman & Esplin (2014) demonstrated that WISE 0855-0714 was roughly midway between those cloudless and cloudy models in a similar diagram of M 4.5 versus J −[4.5], and that its position was best matched by cloudless models that employed nonequilibrium chemistry (Saumon & Marley 2008;Saumon et al 2012). After measuring photometry for WISE 0855-0714 in several additional near-IR bands, Schneider et al (2016) and found that no single suite of models provided a clearly superior match to the observed spectral energy distribution (SED), and that all of the models differed significantly from the data.…”
Section: Discussionmentioning
confidence: 91%