MOCRA: a Monte Carlo code for the simulation of radiative transfer in the atmosphere (Articolo in rivista)

Type
Label
  • MOCRA: a Monte Carlo code for the simulation of radiative transfer in the atmosphere (Articolo in rivista) (literal)
Anno
  • 2012-01-01T00:00:00+01:00 (literal)
Alternative label
  • : Premuda, M (Premuda, Margherita)1; Palazzi, E (Palazzi, Elisa)1; Ravegnani, F (Ravegnani, Fabrizio)1; Bortoli, D (Bortoli, Daniele)1,2; Masieri, S (Masieri, Samuele)1,3; Giovanelli, G (Giovanelli, Giorgio)1 (2012)
    MOCRA: a Monte Carlo code for the simulation of radiative transfer in the atmosphere
    in Optics express
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • : Premuda, M (Premuda, Margherita)1; Palazzi, E (Palazzi, Elisa)1; Ravegnani, F (Ravegnani, Fabrizio)1; Bortoli, D (Bortoli, Daniele)1,2; Masieri, S (Masieri, Samuele)1,3; Giovanelli, G (Giovanelli, Giorgio)1 (literal)
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  • 20 (literal)
Rivista
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  • 7 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • 1. Natl Res Council ISAC CNR, Inst Atmospher Sci & Climate, I-40129 Bologna, Italy 2. Univ Evora CGE UE, Evora Geophys Ctr, P-7000 Evora, Portugal 3. Univ Ca Foscari Venezia Dorsoduro, Venice, Italy (literal)
Titolo
  • MOCRA: a Monte Carlo code for the simulation of radiative transfer in the atmosphere (literal)
Abstract
  • This paper describes the radiative transfer model (RTM) MOCRA (MOnte Carlo Radiance Analysis), developed in the frame of DOAS (Differential Optical Absorption Spectroscopy) to correctly interpret remote sensing measurements of trace gas amounts in the atmosphere through the calculation of the Air Mass Factor. Besides the DOAS-related quantities, the MOCRA code yields: 1- the atmospheric transmittance in the vertical and sun directions, 2- the direct and global irradiance, 3- the single- and multiple-scattered radiance for a detector with assigned position, line of sight and field of view. Sample calculations of the main radiometric quantities calculated with MOCRA are presented and compared with the output of another RTM (MODTRAN4). A further comparison is presented between the NO2 slant column densities (SCDs) measured with DOAS at Evora (Portugal) and the ones simulated with MOCRA. Both comparisons (MOCRA-MODTRAN4 and MOCRA-observations) gave more than satisfactory results, and overall make MOCRA a versatile tool for atmospheric radiative transfer simulations and interpretation of remote sensing measurements. (literal)
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