A linearized discrete ordinate radiative transfer model for atmospheric remote-sensing retrieval

By Robert J. D. Spurr, T. Kurosu, Kelly Chance. 2001

299 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5d0e3ed1ad328cf6db86bd5b8053aa9e6637e084

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

Ozone profile and tropospheric ozone retrievals from the Global Ozone Monitoring Experiment: Algorithm description and validation (2005, methodology): “[18] We use the Linearized Discrete Ordinate Radiative Transfer model (LIDORT) as the forward model to simulate radiances and weighting functions [Spurr et al., 2001].”
The ACOS CO 2 retrieval algorithm – Part 1: Description and validation against synthetic observations (2011, methodology): “Monochromatic radiative transfer calculations are made using a combination of a fast single-scattering model (Nakajima and Tanaka, 1988), the LIDORT scalar multiplescattering model (Spurr et al., 2001), and a second-order-ofscattering polarization model called 2OS (Natraj and Spurr, 2007).”
Anthropogenic emissions of highly reactive volatile organic compounds in eastern Texas inferred from oversampling of satellite (OMI) measurements of HCHO columns (2014, methodology): “The air mass factor (AMF = SCD/VCD) to convert SCD to vertical column density (VCD, column hereafter) is computed following Palmer et al (2001) with the LIDORT radiative transfer model (Spurr et al 2001).”
VLIDORT: A linearized pseudo-spherical vector discrete ordinate radiative transfer code for forward model and retrieval studies in multilayer multiple scattering media (2006, methodology): “The original LIDORT code [28] generated Jacobians and radiances for the top of atmosphere (TOA) reflectance scenario for a plane-parallel multilayer atmosphere.”
Simultaneous derivation of intensities and weighting functions in a general pseudo-spherical discrete ordinate radiative transfer treatment (2002, methodology): “The linearization of the boundary value problem follows in Section 4.5; the treatment is more general than the plane-parallel analysis presented in SKC.”
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”
Global inventory of nitrogen oxide emissions constrained by space‐based observations of NO2 columns (2003, unknown): “scene (Goddard Earth Observing System, (GEOS)-CHEM model, see Appendix A), while the scattering weights are calculated from the Linearized Discrete Ordinate Radiative Transfer (LIDORT) model [Spurr et al., 2001].”