An atmospheric radiative transfer model, code, or simulator calculates radiative transfer of electromagnetic radiation through a planetary atmosphere.

Methods

At the core of a radiative transfer model lies the radiative transfer equation that is numerically solved using a solver such as a discrete ordinate method or a Monte Carlo method. The radiative transfer equation is a monochromatic equation to calculate radiance in a single layer of the Earth's atmosphere. To calculate the radiance for a spectral region with a finite width (e.g., to estimate the Earth's energy budget or simulate an instrument response), one has to integrate this over a band of frequencies (or wavelengths). The most exact way to do this is to loop through the frequencies of interest, and for each frequency, calculate the radiance at this frequency. For this, one needs to calculate the contribution of each spectral line for all molecules in the atmospheric layer; this is called a line-by-line calculation. For an instrument response, this is then convolved with the spectral response of the instrument.

A faster but more approximate method is a band transmission. Here, the transmission in a region in a band is characterised by a set of pre-calculated coefficients (depending on temperature and other parameters). In addition, models may consider scattering from molecules or particles, as well as polarisation; however, not all models do so.

Applications

Radiative transfer codes are used in broad range of applications. They are commonly used as forward models for the retrieval of geophysical parameters (such as temperature or humidity). Radiative transfer models are also used to optimize solar photovoltaic systems for renewable energy generation. Another common field of application is in a weather or climate model, where the radiative forcing is calculated for greenhouse gases, aerosols, or clouds. In such applications, radiative transfer codes are often called radiation parameterization. In these applications, the radiative transfer codes are used in forward sense, i.e. on the basis of known properties of the atmosphere, one calculates heating rates, radiative fluxes, and radiances.

There are efforts for intercomparison of radiation codes. One such project was ICRCCM (Intercomparison of Radiation Codes in Climate Models) effort that spanned the late 1980s – early 2000s. The more current (2011) project, Continual Intercomparison of Radiation Codes, emphasises also using observations to define intercomparison cases.

Table of models

NameWebsiteReferencesUVVisibleNear IRThermal IRmm/sub-mmMicrowaveline-by-line/bandScatteringPolarisedGeometryLicenseNotes
4A/OP2011-07-21 at the Wayback MachineScott and Chédin (1981)NoNoYesYesNoNoband or line-by-lineYesYesfreeware
6S/6SV1Kotchenova et al. (1997)NoYesYesNoNoNoband?Yesnon-Lambertian surface
ARTSEriksson et al. (2011) Buehler et al. (2018)NoNoNoYesYesYesline-by-lineYesYesspherical 1D, 2D, 3DGPL
BTRAMChapman et al. (2009)NoYesYesYesYesYesline-by-lineNoNo1D, plane-parallelproprietary commercial
COARTJin et al. (2006)YesYesYesYesNoNoYesNoplane-parallelfree
CMFGENHillier (2020)YesYesYesYesYesYesline-by-lineYesYes1D
CRMNoYesYesYesNoNobandYesNofreely availablePart of NCAR Community Climate Model
CRTMJohnson et al. (2023)v3.0YesYesYesYespassive, activebandYesv3.0, UV/VIS1D, Plane-ParallelPublic DomainFresnel ocean surfaces, Lambertian non-ocean surface
DART radiative transfer modelGastellu-Etchegorry et al. (1996)NoYesYesYesNoNobandYes?spherical 1D, 2D, 3Dfree for research with licensenon-Lambertian surface, landscape creation and import
DISORTStamnes et al. (1988) Lin et al. (2015)YesYesYesYesYesradarYesNoplane-parallel or pseudo-spherical (v4.0)free with restrictionsdiscrete ordinate, used by others
EradiateNoYesYesNoNoNoband or line-by-lineYesNoplane-parallel, sphericalLGPL3D surface simulation
FARMSXie et al. (2016)λ>0.2 µmYesYesNoNoNobandYesNoplane-parallelfreeRapidly simulating downwelling solar radiation at land surface for solar energy and climate research
Fu-LiouFu and Liou (1993)NoYesYes?NoNoYes?plane-parallelusage online, source code availableweb interface online at
FUTBOLINMartin-Torres (2005)λ>0.3 µmYesYesYesλ<1000 µmNoline-by-lineYes?spherical or plane-parallelhandles line-mixing, continuum absorption and NLTE
GENLN2Edwards (1992)???Yes??line-by-line??
KARINEEymet (2005)NoNoYesNoNo??plane-parallelGPL
KCARTA??YesYes??line-by-lineYes?plane-parallelfreely availableAIRS reference model
KOPRANoNoNoYesNoNo??
LBLRTMClough et al. (2005)YesYesYesYesYesYesline-by-line??
LEEDRFiorino et al. (2014)λ>0.2 µmYesYesYesYesYesband or line-by-lineYes?sphericalUS government softwareextended solar & lunar sources; single & multiple scattering
Gordley et al. (1994)YesYesYesYesYesYesline-by-lineNoNospherical (Earth and Mars), plane-parallelfreely available with restrictionsweb interface,
libRadtranMayer and Kylling (2005)YesYesYesYesNoNoband or line-by-lineYesYesplane-parallel or pseudo-sphericalGPL
MATISSECaillault et al. (2007)NoYesYesYesNoNobandYes?proprietary freeware
MCARaTSGPL3-D Monte Carlo
MODTRANBerk et al. (1998)<50,000 cm−1 (eq. to λ>0.2 µm)YesYesYesYesYesband or line-by-lineYes?proprietary commercialsolar and lunar source, uses DISORT
MOSARTCornette (2006)λ>0.2 µmYesYesYesYesYesbandYesNofreely available
MSCARTWang et al. (2017) Wang et al. (2019)YesYesYesNoNoNoYesYes1D, 2D, 3Davailable on request
PICASOBatalha et al. (2019) Mukherjee et al. (2022)λ>0.3 μmYesYesYesNoNoband or correlated-kYesNoplane-parallel, 1D, 3Dexoplanet, brown dwarf, climate modeling, phase-dependence
PUMASYesYesYesYesYesYesLine-by-line and correlated-kYesYesplane-parallel and pseudo-sphericalFree/online tool
RADISPannier (2018)NoNoYesNoNoNoNo1DGPL
RFMNoNoNoYesNoNoline-by-lineNo?available on requestMIPAS reference model based on GENLN2
RRTM/RRTMGMlawer, et al. (1997)<50,000 cm−1 (eq. to λ>0.2 µm)YesYesYesYes>10 cm−1??free of chargeuses DISORT
RTMOM[dead link]λ>0.25 µmYesYesλ<15 µmNoNoline-by-lineYes?plane-parallelfreeware
RTTOVSaunders et al. (1999)λ>0.4 µmYesYesYesYesYesbandYes?available on request
SASKTRANBourassa et al. (2008)Zawada et al.(2015)YesYesYesNoNoNoline-by-lineYesYesspherical 1D, 2D, 3D, plane-parallelavailable on requestdiscrete and Monte Carlo options
SBDARTRicchiazzi et al. (1998)YesYesYes?NoNoYes?plane-paralleluses DISORT
SCIATRANRozanov et al. (2005) , Rozanov et al. (2014)YesYesYesNoNoNoband or line-by-lineYesYesplane-parallel or pseudo-spherical or spherical
SHARMLyapustin (2002)NoYesYesNoNoNoYes?
SHDOMEvans (2006)??YesYes??Yes?
σ-IASIAmato et al. (2002)NoNoYesYesYesNoband, based on LBLRTM v12.4YesNoplane-parallelSource code available online. Free for non commercial purposes.Analytical Jacobians. Complex treatment of aerosols/clouds with Tang scheme.
SMART-GRamon et al. (2019)YesYesYesNoNoNoband or line-by-lineYesYesplane-parallel or sphericalfree for non-commercial purposesMonte-Carlo code parallelized by GPU (CUDA). Atmosphere or/and ocean options
Streamer, FluxnetKey and Schweiger (1998)NoNoλ>0.6 mmλ<15 mmNoNobandYes?plane-parallelFluxnet is fast version of STREAMER using neural nets
XRTMYesYesYesYesYesYesYesYesplane-parallel and pseudo-sphericalGPL
VLIDORT/LIDORTSpurr and Christi (2019)YesYesYesYes??line-by-lineYesYes VLIDORT onlyplane-parallelUsed in SMART and VSTAR radiative transfer
NameWebsiteReferencesUVVISNear IRThermal IRMicrowavemm/sub-mmline-by-line/bandScatteringPolarisedGeometryLicenseNotes

Molecular absorption databases

For a line-by-line calculation, one needs characteristics of the spectral lines, such as the line centre, the intensity, the lower-state energy, the line width and the shape.

NameAuthorDescription
HITRANRothman et al. (1987, 1992, 1998, 2003, 2005, 2009, 2013, 2017)HITRAN is a compilation of molecular spectroscopic parameters that a variety of computer codes use to predict and simulate the transmission and emission of light in the atmosphere. The original version was created at the Air Force Cambridge Research Laboratories (1960's). The database is maintained and developed at the Harvard-Smithsonian Center for Astrophysics in Cambridge MA, USA.
GEISAJacquinet-Husson et al. (1999, 2005, 2008)GEISA (Gestion et Etude des Informations Spectroscopiques Atmosphériques: Management and Study of Spectroscopic Information) is a computer-accessible spectroscopic database, designed to facilitate accurate forward radiative transfer calculations using a line-by-line and layer-by-layer approach. It was started in 1974 at Laboratoire de Météorologie Dynamique (LMD/IPSL) in France. GEISA is maintained by the ARA group at LMD (Ecole Polytechnique) for its scientific part and by the ETHER group (CNRS Centre National de la Recherche Scientifique-France) at IPSL (Institut Pierre Simon Laplace) for its technical part. Currently, GEISA is involved in activities related to the assessment of the capabilities of IASI (Infrared Atmospheric Sounding Interferometer on board of the METOP European satellite) through the GEISA/IASI database derived from GEISA.

See also

Footnotes

General

  • Bohren, Craig F. and Eugene E. Clothiaux, Fundamentals of atmospheric radiation: an introduction with 400 problems, Weinheim: Wiley-VCH, 2006, 472 p., ISBN 3-527-40503-8.
  • Goody, R. M. and Y. L. Yung, Atmospheric Radiation: Theoretical Basis. Oxford University Press, 1996 (Second Edition), 534 pages, ISBN 978-0-19-510291-8.
  • Liou, Kuo-Nan, An introduction to atmospheric radiation, Amsterdam; Boston: Academic Press, 2002, 583 p., International geophysics series, v.84, ISBN 0-12-451451-0.
  • Mobley, Curtis D., Light and water: radiative transfer in natural waters; based in part on collaborations with Rudolph W. Preisendorfer, San Diego, Academic Press, 1994, 592 p., ISBN 0-12-502750-8
  • Petty, Grant W, A first course in atmospheric radiation (2nd Ed.), Madison, Wisconsin: Sundog Pub., 2006, 472 p., ISBN 0-9729033-1-3
  • Preisendorfer, Rudolph W., Hydrologic optics, Honolulu, Hawaii: U.S. Dept. of Commerce, National Oceanic & Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1976, 6 volumes.
  • Stephens, Graeme L., Remote sensing of the lower atmosphere: an introduction, New York, Oxford University Press, 1994, 523 p. ISBN 0-19-508188-9.
  • Thomas, Gary E. and Knut Stamnes, Radiative transfer in the atmosphere and ocean, Cambridge, New York, Cambridge University Press, 1999, 517 p., ISBN 0-521-40124-0.
  • Zdunkowski, W., T. Trautmann, A. Bott, Radiation in the Atmosphere. Cambridge University Press, 2007, 496 pages, ISBN 978-0-521-87107-5

External links