Radiative Transfer in the Atmosphere and Ocean

By Timo Vesala. 2003

342 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/684a21a7a321e730cc8db773c43dc663e3e582ce

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Citations in the corpus

Simultaneous derivation of intensities and weighting functions in a general pseudo-spherical discrete ordinate radiative transfer treatment (2002, methodology): “The advantages of the double quadrature scheme have been discussed in the literature (see for example [21]).”
The HITRAN molecular spectroscopic database: edition of 2000 including updates through 2001 (2003, background): “For an atmosphere that has particles that scatter as well as absorb, radiative transfer in the atmosphere is described by a source function that has both thermal emission and scattering terms [159].”
Effects of the physical state of tropospheric ammonium-sulfate-nitrate particles on global aerosol direct radiative forcing (2003, neutral): “Random overlap of stratus clouds is assumed (Morcrette and Fouquart, 1986; Briegleb, 1992; Thomas and Stamnes, 1999).”
One Martian year of atmospheric observations using MER Mini‐TES (2006, methodology): “The synthetic spectrum is computed using a two-stream radiative transfer code that includes aerosol scattering [e.g., Goody and Yung, 1989; Thomas and Stamnes, 1999 ].”
Next-generation angular distribution models for top-of-atmosphere radiative flux calculation from CERES instruments: validation (2015, methodology): “BRDF and α is the clear-sky spherical albedo (Thomas and Stamnes, 1999), and they are derived from 1× 1 BRDF fits (Sect.”
VLIDORT: A linearized pseudo-spherical vector discrete ordinate radiative transfer code for forward model and retrieval studies in multilayer multiple scattering media (2006, methodology): “For each Fourier term m, the multiple scatter integral over the upper and lower polar direction half-spaces is approximated by a double Gaussian quadrature scheme [54], with stream directions {7mi} and Gauss–Legendre weights {wi} for i 1⁄4 1,yN.”
Empirical studies of cloud effects on UV radiation: A review (2005, background): “However, most international agencies and consortia agree in establishing this boundary at 315 nm: World Health Organization (WHO) [2002]; European Union’s action COST 713 [Vanicek et al., 2000]; Commission Internationale de l’Eclairage [1999]; and International Agency for Research on Cancer [1992]. ”
Optical properties of terrestrial clouds (2004, methodology): “They also can be used to check the accuracy of new algorithms using the fact that the numerical solution of the radiative transfer equation (Thomas and Stamnes, 1999) and results presented above for optically thick layers should converge as s!l and b!”
Improved scattering radiative transfer for frozen hydrometeors at microwave frequencies (2014, methodology): “As a variant of the two-stream solution, the delta-Eddington method might appear crude in comparison to the many other solvers available (e.g.Thomas and Stamnes, 1999).”
In-situ measured spectral directional emissivity of snow and ice in the 8-14 μm atmospheric window (2006, background): “…TIR are derived from the measured directional emissivity (() at h ext = 45-using Kirchhoff's law given by q(k, À h ext , 2p) = 1 À ((k, h ext ), where q(k, À h ext , 2p) is the directional – hemispherical reflectance (DHR) for the wavelength k at the incidence angle h ext (Thomas & Stamnes, 1999).”