MORLEY ET AL. 2012: T/Y DWARF MODELS
Model photometry and spectra currently available. These models include Na2S, KCl, ZnS, MnS, and Cr clouds. Models have effective temperatures from 400 to 1200 K, gravities from log g(cgs) 4.0 to 5.5. These models are especially appropriate for late T dwarfs cooler than ~900 K (spectral type ~T9). We calculate Vega absolute magnitudes for Y, J, H, K, L’, M’ (all MKO), IRAC bands 1-4, and WISE bands 1-4. Other filters available upon request.
MORLEY ET AL. 2014: Y DWARF MODELS
These models include H2O ice clouds in addition to the Na2S, KCl, ZnS, MnS, and Cr clouds. Models have effective temperatures from 200 to 450 K, gravities from log g(cgs) 3.0 to 5.0. These models are partly cloudy (see Morley et al. 2014): we assume that 50% of the surface is covered in clouds. We calculate Vega absolute magnitudes for Y, J, H, K, L', M' (all MKO), IRAC bands 1-4, and WISE bands 1-4. Other filters available upon request.
SAUMON ET AL. 2012: CLOUD-FREE MODELS FOR T DWARFS
Model photometry and spectra currently available. These models do not include cloud opacity. Models have effective temperatures from 200 to 1200 K, gravities from log g(cgs) 4.0 to 5.5. These models are appropriate for mid-late T dwarfs cooler than ~1100-1200 K (spectral type ~T3). Note that L dwarfs and early T dwarfs require models that include iron/silicate clouds (photometry not available here). We calculate Vega absolute magnitudes for Y, J, H, K, L’, M’ (all MKO), IRAC bands 1-4, and WISE bands 1-4. Other filters available upon request.
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