SMARTS (The Simple Model of the Atmospheric Radiative Transfer of Sunshine)
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The Simple Model of the Atmospheric Radiative Transfer of Sunshine (SMARTS) is a computer program designed to evaluate the surface solar irradiance components in the shortwave spectrum (spectral range 280 to 4000 nm) under cloudless conditions. The program, written in FORTRAN, relies on simplifications of the equation of
radiative transfer Radiative transfer is the physical phenomenon of energy transfer in the form of electromagnetic radiation. The propagation of radiation through a medium is affected by absorption, emission, and scattering processes. The equation of radiative trans ...
to allow extremely fast calculations of the surface irradiance. The irradiance components can be incident on a horizontal, a fixed-tilt or a 2-axis tracking surface. SMARTS can be used for example to evaluate the energy production of solar panels under variable atmospheric conditions. Many other applications are possible.


History

The first versions of SMARTS were developed by Dr. Gueymard while he was at the
Florida Solar Energy Center The Florida Solar Energy Center (FSEC) is a research institute of the University of Central Florida, located on a 20-acre (.08 km2) research complex on Florida's Space Coast at UCF's Cocoa satellite campus. FSEC is the largest and most act ...
. The model employed a structure similar to the earlier SPCTRAL2 model, still offered b
the National Renewable Energy Laboratory
(
NREL The National Renewable Energy Laboratory (NREL) in the US specializes in the research and development of renewable energy, energy efficiency, energy systems integration, and sustainable transportation. NREL is a federally funded research and ...
), but with finer spectral resolution, as well as updated extraterrestrial spectrum and transmittance functions. The latter consisted mostly of parameterizations of results obtained with MODTRAN. The latest versions (2.9.2 and 2.9.5) of SMARTS are hosted b
NREL
The program can be freely downloaded but is subject to a License Agreement, which limits its use to civilian research and education. For new users, an optional graphical interface (for Windows OS only) is available to ease the preparation of the input file. Program packages are available for the Windows, Macintosh, and Linux platforms.


Applications

SMARTS version 2.9.2 was selected to prepare various reference terrestrial spectra, which have been standardized by ASTM under the designations G173, G177 and G197, and by IEC under 60904-3. The latter standard represents the spectral distribution of global irradiance incident on a 37° tilted surface facing the sun at an
air mass In meteorology, an air mass is a volume of air defined by its temperature and humidity. Air masses cover many hundreds or thousands of square miles, and adapt to the characteristics of the surface below them. They are classified according to l ...
of 1.5. The integrated irradiance amounts to 1000 W/m2. This standard spectrum is mandated by IEC to evaluate the rating of photovoltaic (PV) solar cells in the absence of optical concentration. PV cells requiring concentration referred to as CPV cells are normally evaluated against the direct spectrum at air mass 1.5 described in ASTM G173. This spectrum integrates to 900 W/m2. The reasons behind the selection of the atmospheric and environmental conditions that eventually led to the development of ASTM G173 are described in a scientific paper. SMARTS version 2.9.2 is considered an adjunct standard to G173 by ASTM. Further details on the use of SMARTS for PV or CPV applications are available in other publications. In particular, the model is frequently used to evaluate real-world efficiencies of PV or CPV modules and evaluate mismatch factors. The reference spectra in ASTM G197 have been developed to evaluate the optical characteristics of fenestration devices when mounted vertically (windows) or on structures inclined at 20° from the horizontal (skylights on roofs). The reference spectrum in ASTM G177 is limited to the global irradiance in the ultraviolet (280–400 nm), and corresponds to "high-UV" conditions frequently encountered in arid and elevated sites, such as in the southwest USA. This spectrum is to be used as a reference for testing the degradation and durability of materials.


Features

The program uses various inputs that describe the atmospheric conditions for which the irradiance spectra are to be calculated. Ideal conditions, based on various possible model atmospheres and aerosol models, can be selected by the user. Alternatively, realistic conditions can also be specified as inputs, based for example on aerosol and water vapor data provided by a sunphotometer. In turn, these realistic conditions are necessary to compare the modeled spectra to those measured by a
spectroradiometer A spectroradiometer is a light measurement tool that is able to measure both the wavelength and amplitude of the light emitted from a light source. Spectrometers discriminate the wavelength based on the position the light hits at the detector array ...
. Reciprocally, since the model is well validated, this comparative method can be used as guidance to detect malfunction or miscalibration of instruments.R. Galleano, W. Zaaiman, A. Virtuani, D. Pavanello, P. Morabito, A. Minuto, A. Spena, S. Bartocci, R. Fucci, G. Leanza, D. Fasanaro and M. Catena, Intercomparison campaign of spectroradiometers for a correct estimation of solar spectral irradiance: results and potential impact on photovoltaic devices calibration. Prog. Photovolt., DOI: 10.1002/pip.2361 (2013). The original spectral resolution of the model is 0.5 nm in the UV, 1 nm in the visible and near-infrared, and 5 nm above 1700 nm. To facilitate comparisons between the modeled spectra and actual measurements at a different spectral resolution, the SMARTS post-processor may be used to smooth the modeled spectra and adapt them to simulate the optical characteristics of a specific spectroradiometer. Additionally, the model provides the spectrally-integrated (or "broadband") irradiance values, which can then be compared to measurements from a
pyrheliometer A pyrheliometer is an instrument for measurement of direct beam solar irradiance. Sunlight enters the instrument through a window and is directed onto a thermopile which converts heat to an electrical signal that can be recorded. The signal vo ...
(for direct radiation) or
pyranometer A pyranometer is a type of actinometer used for measuring solar irradiance on a planar surface and it is designed to measure the solar radiation flux density (W/m2) from the hemisphere above within a wavelength range 0.3 μm to 3 μm. The name pyra ...
(for diffuse or global radiation) at any instant. Besides the atmospheric conditions, another important input is the solar geometry, which can be defined by the sun position (
zenith The zenith (, ) is an imaginary point directly "above" a particular location, on the celestial sphere. "Above" means in the vertical direction ( plumb line) opposite to the gravity direction at that location ( nadir). The zenith is the "high ...
angle and
azimuth An azimuth (; from ar, اَلسُّمُوت, as-sumūt, the directions) is an angular measurement in a spherical coordinate system. More specifically, it is the horizontal angle from a cardinal direction, most commonly north. Mathematical ...
), the air mass, or by specifying the date, time, and location. Optional calculations include the circumsolar irradiance,
illuminance In photometry (optics), photometry, illuminance is the total luminous flux incident on a surface, per unit area. It is a measure of how much the incident light illuminates the surface, wavelength-weighted by the luminosity function to correlate w ...
components,
photosynthetically active radiation Photosynthetically active radiation (PAR) designates the spectral range (wave band) of solar radiation from 400 to 700 nanometers that photosynthetic organisms are able to use in the process of photosynthesis. This spectral region corresponds more o ...
(PAR) components, and irradiance calculations in the UV, involving a variety of action spectra (such as that corresponding to the
erythema Erythema (from the Greek , meaning red) is redness of the skin or mucous membranes, caused by hyperemia (increased blood flow) in superficial capillaries. It occurs with any skin injury, infection, or inflammation. Examples of erythema not asso ...
). The program outputs its results to text files, which can be further imported and processed into spreadsheets. A graphic interface, providing plots of the calculated spectra using National Instruments'
LabVIEW Laboratory Virtual Instrument Engineering Workbench (LabVIEW) is a system-design platform and development environment for a visual programming language from National Instruments. The graphical language is named "G"; not to be confused with G-c ...
software, is als
available


See also

* Air mass (solar energy) *
Atmosphere of Earth The atmosphere of Earth is the layer of gases, known collectively as air, retained by Earth's gravity that surrounds the planet and forms its planetary atmosphere. The atmosphere of Earth protects life on Earth by creating pressure allowing fo ...
*
Concentrated photovoltaics Concentrator photovoltaics (CPV) (also known as concentration photovoltaics) is a photovoltaic technology that generates electricity from sunlight. Unlike conventional photovoltaic systems, it uses lenses or curved mirrors to focus sunlight ont ...
*
Diffuse sky radiation Diffuse sky radiation is solar radiation reaching the Earth's surface after having been scattered from the direct solar beam by molecules or particulates in the atmosphere. It is also called sky radiation, the determinative process for cha ...
*
Electromagnetic radiation and health Electromagnetic radiation can be classified into two types: ionizing radiation and non-ionizing radiation, based on the capability of a single photon with more than 10  eV energy to ionize atoms or break chemical bonds. Extreme ultra ...
*
Illuminance In photometry (optics), photometry, illuminance is the total luminous flux incident on a surface, per unit area. It is a measure of how much the incident light illuminates the surface, wavelength-weighted by the luminosity function to correlate w ...
* Insolation * Irradiance *
List of atmospheric radiative transfer codes 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 ...
* MODTRAN *
Rayleigh scattering Rayleigh scattering ( ), named after the 19th-century British physicist Lord Rayleigh (John William Strutt), is the predominantly elastic scattering of light or other electromagnetic radiation by particles much smaller than the wavelength of th ...
* Sunlight * Sunshine


References

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External links

* Official website : http://www.solarconsultingservices.com/smarts.php * Download website : http://www.nrel.gov/rredc/smarts/ Electromagnetic radiation Atmospheric radiative transfer codes