Atmospheric Chemistry in Giant Planets, Brown Dwarfs, and Low-Mass Dwarf Stars: I. Carbon, Nitrogen, and Oxygen
By K. Lodders, B. Fegley. 2002
367 citations recorded by the source corpus.
Subfields: Atmospheric Science, Atomic and Molecular Physics, and Optics, Organic Chemistry
View Paper: https://www.semanticscholar.org/paper/aa72e65c6066a8dfd3dd16af49f6bad9cc2f5fc4
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Citations in the corpus
- Temperature–pressure profile of the hot Jupiter HD 189733b from HST sodium observations: detection of upper atmospheric heating (2012, neutral): “The solar abundance ratio of sodium to water is ξNa/ξH2O[solar] = 6.63−9.95×10−3 or ln(ξNa/ξH2O[solar]) = −5.0 to −4.6 (Lodders 2003; Lodders & Fegley 2002; Sharp & Burrows 2007).”
- On the Cool Side: Modeling the Atmospheres of Brown Dwarfs and Giant Planets (2014, methodology): “Examples of equilibrium gas abundances, or ratios of gas abundances, for several key species of interest (from the rainout models of Lodders & Fegley 2002; Visscher et al. 2006) are shown in Figure 3, along with model temperature profiles for a few representative objects.”
- Comparative Planetary Atmospheres: Models of TrES-1 and HD 209458b (2005, methodology): “We use the elemental abundance data of Lodders (2003) and compute chemical equilibrium compositions following Fegley & Lodders (1994) and Lodders & Fegley (2002).”
- Titanium and Vanadium Chemistry in Low-Mass Dwarf Stars (2002, methodology): “Chemical equilibrium computations were done using the CONDOR code, which is described in detail elsewhere (e.g., Fegley & Lodders 1994; Lodders & Fegley 2002).”
- On the Luminosity of Young Jupiters (2006, methodology): “We use the elemental abundance data of Lodders (2003) and compute chemical equilibrium compositions following Fegley & Lodders (1994), Lodders & Fegley (2002), and Lodders (2002).”
- HST PanCET Program: A Cloudy Atmosphere for the Promising JWST Target WASP-101b (2017, background): “These models account for condensation and thermal ionization, though do not include photochemistry (Lodders 1999; Lodders & Fegley 2002; Lodders 2002; Visscher A Cloudy Atmosphere for WASP-101b 5 WASP-101b WASP-31b WASP-17b WASP-101b WASP-31b WASP-17b WASP-101b WASP-31b WASP-17b Al2O3 Fe MgSiO3 Cr…”
- The Evolution of L and T Dwarfs in Color-Magnitude Diagrams (2008, methodology): “Our chemical equilibrium grid of molecular, atomic, and ionic abundances as a function of temperature, pressure, and metallicity is based on the work of Fegley & Lodders (1994,1996), Lodders (1999, 2002), and Lodders & Fegley (2002, 2006).”
- A Spitzer Infrared Spectrograph Spectral Sequence of M, L, and T Dwarfs (2004, background): “The changes in the spectral morphology across the MLT sequence illustrate all of the major chemical transitions expected to occur in the atmospheres of ultracool dwarfs (Fegley & Lodders 1996; Lodders 1999; Burrows & Sharp 1999; Lodders & Fegley 2002).”
- Spitzer IRAC Photometry of M, L, and T Dwarfs (2006, positive): “More recently, the models have begun to take into account nonequilibrium chemistry (e.g., Noll et al. 1997; Saumon et al. 2000, 2003, 2006; Burrows et al. 2000; Ackerman & Marley 2001; Allard et al. 2001; Lodders & Fegley 2002; Marley et al. 2002; Tsuji 2002).”
- NEGLECTED CLOUDS IN T AND Y DWARF ATMOSPHERES (2012, methodology): “The abundances of molecular, atomic, and ionic species are calculated using thermochemical equilibrium following the models of Fegley & Lodders (1994, 1996); Lodders (1999); Lodders & Fegley (2002); Lodders (2002, 2003); Lodders & Fegley (2006); Lodders (2009).”
- New spectral types L and T (2005, methodology): “For more information on this topic, the reader is referred to the detailed papers by Lodders (2002) and Lodders & Fegley (2002) and the review by Burrows et al. (2001).”
- TRANSITIONS IN THE CLOUD COMPOSITION OF HOT JUPITERS (2016, methodology): “We use the opacities described in Freedman et al. (2008), including more recent updates (Freedman et al. 2014), and the molecular abundances described by Lodders & Fegley (2002) and Visscher et al. (2006).”
- Atmosphere, Interior, and Evolution of the Metal-rich Transiting Planet HD 149026b (2005, methodology): “The specifics of CO and CH4 abundances are discussed in detail in Lodders & Fegley (2002).”
- Atomic and Molecular Opacities for Brown Dwarf and Giant Planet Atmospheres (2006, background): “Extensive updates to these thermodynamic databases have been made by Lodders & Fegley (2002).”
- TRANSMISSION SPECTRA OF THREE-DIMENSIONAL HOT JUPITER MODEL ATMOSPHERES (2009, methodology): “The equilibrium chemistry mixing ratios (Lodders & Fegley 2002, 2006; Lodders 2009) are paired with the opacity database (Freedman et al. 2008) to generate pressure-, temperature-, and wavelength-dependent absorption cross-sections that are used for that particular column.”
- CLOUDS AND CHEMISTRY IN THE ATMOSPHERE OF EXTRASOLAR PLANET HR8799b (2011, background): “The reaction time scales (in seconds) for N2 → NH3 and CO → CH4 are from Lodders & Fegley (2002) and Yung et al. (1988), respectively: τN2 = 1 κN2N(H2) (1) κN2 = 8.45× 10 −8exp ( −81515 T ) (2) τCO = N(CO) κ7N(H)N(H2CO) (3) where T is the gas temperature in Kelvin, κ are the rate coefficients in…”
- VULCAN: An Open-source, Validated Chemical Kinetics Python Code for Exoplanetary Atmospheres (2016, background): “…of work on the atmospheric chemistry of exoplanets, and the published models fall into two basic groups: chemical equilibrium (Burrows & Sharp 1999; Lodders & Fegley 2002; Madhusudhan 2012; Blecic et al. 2016) and photochemical kinetics (Kopparapu, Kasting & Zahnle 2012; Line et al. 2011; Visscher…”
- THE DEUTERIUM-BURNING MASS LIMIT FOR BROWN DWARFS AND GIANT PLANETS (2010, background): “…al. 2001, 2003; Baraffe et al. 2002, 2003; Allard et al. 2003; Chabrier et al. 2000b,a; Chabrier & Baraffe 2000; Sharp & Burrows 2007; Barman 2008) and sophisticated chemical models (Fegley & Lodders 1994; Lodders & Fegley 2002; Burrows & Sharp 1999; Sharp & Burrows 2007; Allard & Hauschildt 1995).”
- A Possible Bifurcation in Atmospheres of Strongly Irradiated Stars and Planets (2003, background): “However, thermochemical equilibrium calculations with rainout (Burrows & Sharp 1999; Lodders & Fegley 2002) suggest that TiO and VO would exist at such high-T/low-P points.”