Simultaneous derivation of intensities and weighting functions in a general pseudo-spherical discrete ordinate radiative transfer treatment

By Robert J. D. Spurr. 2002

136 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4da62ac5c720286577c273665bde4acd73d1091e

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Citations in the corpus

Effects of the physical state of tropospheric ammonium-sulfate-nitrate particles on global aerosol direct radiative forcing (2003, unknown): “This pseudo-spherical approximation is essential for high solar zenith angles (Dahlback and Stamnes, 1991; Spurr, 2002).”
Ozone profile and tropospheric ozone retrievals from the Global Ozone Monitoring Experiment: Algorithm description and validation (2005, methodology): “The version of LIDORT used here implements the pseudospherical approximation [Spurr, 2002] for the direct-beam attenuation, which enables the backscattered radiances to be accurately obtained for a range of Solar Zenith Angles (SZAs) up to 90 within 0.3% in the nadir direction [Caudill et al.,…”
Remote sensed and in situ constraints on processes affecting tropical tropospheric ozone (2006, methodology): “Coincident NO2 and HCHO shape factors are from the modified GEOS-Chem simulation described in Sect.3.”
VLIDORT: A linearized pseudo-spherical vector discrete ordinate radiative transfer code for forward model and retrieval studies in multilayer multiple scattering media (2006, methodology): “These expressions have counterparts in the scalar code (see for example [29]).”
Planetary Spectrum Generator: An accurate online radiative transfer suite for atmospheres, comets, small bodies and exoplanets (2018, methodology): “tes formulation computes the diffuse radiation field for a plane-parallel atmosphere. When spherical geometry is important (e.g., limb geometry observations), the pseudospherical approximation (e.g., [81,86]) is used for computational efficiency. In this scheme, the source functions computed using t”
Evaluation of space‐based constraints on global nitrogen oxide emissions with regional aircraft measurements over and downwind of eastern North America (2006, methodology): “model simulation of that scene, while the scattering weights are calculated from the Linearized Discrete Ordinate Radiative Transfer (LIDORT) model [Spurr et al., 2001; Spurr, 2002].”
Multi-model ensemble simulations of tropospheric NO2 compared with GOME retrievals for the year 2000 (2006, unknown): “Retrieval aspect BIRA/KNMI University of Bremen Dalhousie/SAO Spectral fit DOAS (426.3–451.3 nm) DOAS (425–450 nm) Direct spectral fit (426–452 nm) Stratosphere-troposphere separation Data assimilation in the TM4 model Reference sector method: stratospheric contribution from daily output at GOME ove”