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@@ -173,6 +173,36 @@ The easier way to to use `~pysynphot.catalog.Icat` (also see
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>>> sp = S.Icat('k93models', 10000, 0.1, 3.0)
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.. _pysynphot-appendixa-phoenix:
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Phoenix Models
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==============
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The ``$PYSYN_CDBS/grid/phoenix`` directory contains models provided by
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`F. Allard et al. <http://perso.ens-lyon.fr/france.allard/>`_
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and can be found in the
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`Star, Brown Dwarf, and Planet Simulator <http://phoenix.ens-lyon.fr/simulator/index.faces>`_. They use static, spherical symmetric, 1D simulations to completely
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describe the atmospheric emission spectrum. The models account for the
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formation of molecular bands, such as those of water vapor, methane, or
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titanium dioxide, solving for the transfer equation over more than 20,000
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wavelength points on average, producing synthetic spectra with 2 Angstroms
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resolution. The line selection is repeated at each iteration of the model
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until it has converged and the thermal structure obtained. The models here
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are calculated with a cloud model, valid across the entire parameter range.
The atlas data files are organized in a similar naming convention as
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:ref:`pysynphot-appendixa-kurucz1993`, and are easily accessible using
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`~pysynphot.catalog.Icat` (also see :ref:`pysynphot-spec-atlas`).
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The example below generates a spectrum with metallicity :math:`\log Z = +0.1`,
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temperature :math:`T_{\textnormal{eff}} = 10000\textnormal{K}`, and gravity
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:math:`\log g = 3.0`:
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>>> sp = S.Icat('phoenix', 10000, 0.1, 3.0)
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.. _pysynphot-appendixa-calspec:
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HST Calibration Spectra
@@ -398,36 +428,6 @@ The example below loads a source spectrum of spectral type G0V from the atlas:
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>>> sp = S.FileSpectrum(filename)
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.. _pysynphot-appendixa-phoenix:
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Phoenix Models
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==============
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The ``$PYSYN_CDBS/grid/phoenix`` directory contains models provided by
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`F. Allard et al. <http://perso.ens-lyon.fr/france.allard/>`_
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and can be found in the
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`Star, Brown Dwarf, and Planet Simulator <http://phoenix.ens-lyon.fr/simulator/index.faces>`_. They use static, spherical symmetric, 1D simulations to completely
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describe the atmospheric emission spectrum. The models account for the
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formation of molecular bands, such as those of water vapor, methane, or
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titanium dioxide, solving for the transfer equation over more than 20,000
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wavelength points on average, producing synthetic spectra with 2 Angstroms
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resolution. The line selection is repeated at each iteration of the model
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until it has converged and the thermal structure obtained. The models here
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-
are calculated with a cloud model, valid across the entire parameter range.
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