ASTM G173 - 03(2012)

    Standard Tables for Reference Solar Spectral Irradiances: Direct Normal and Hemispherical on 37° Tilted Surface

    Active Standard ASTM G173 | Developed by Subcommittee: G03.09

    Book of Standards Volume: 14.04

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    Significance and Use

    4.1 Absorptance, reflectance, and transmittance of solar energy are important factors in material degradation studies, solar thermal system performance, solar photovoltaic system performance, biological studies, and solar simulation activities. These optical properties are normally functions of wavelength, which require the spectral distribution of the solar flux be known before the solar-weighted property can be calculated. To compare the relative performance of competitive products, or to compare the performance of products before and after being subjected to weathering or other exposure conditions, a reference standard solar spectral distribution is desirable.

    4.2 These tables provide appropriate standard spectral irradiance distributions for determining the relative optical performance of materials, solar thermal, solar photovoltaic, and other systems. The tables may be used to evaluate components and materials for the purpose of solar simulation where either the direct or the hemispherical (that is, direct beam plus diffuse sky) spectral solar irradiance is desired. However, these tables are not intended to be used as a benchmark for ultraviolet radiation used in indoor exposure testing of materials using manufactured light sources.

    4.3 The total integrated irradiances for the direct and hemispherical tilted spectra are 900.1 W·m-2 and 1000.4 W·m-2, respectively. Note that, in PV applications, no amplitude adjustments are required to match standard reporting condition irradiances of 1000 W·m-2 for hemispherical irradiance.

    4.4 Previously defined global hemispherical reference spectrum (G159) for a sun-facing 37°-tilted surface served well to meet the needs of the flat plate photovoltaic research, development, and industrial community. Investigation of prevailing conditions and measured spectra shows that this global hemispherical reference spectrum can be attained in practice under a variety of conditions, and that these conditions can be interpreted as representative for many combinations of atmospheric parameters. Earlier global hemispherical reference spectrum may be closely, but not exactly, reproduced with improved spectral wavelength range, uniform spectral interval, and spectral resolution equivalent to the spectral interval, using inputs in X1.4.

    4.5 Reference spectra generated by the SMARTS Version 2.9.2 model for the indicated conditions are shown in Fig. 1. The exact input file structure required to generate the reference spectra is shown in Table 1.

    Plot of Direct Normal Spectral Irradiance (Solid Line)
and Hemispherical Spectral Irradiance on 37° Tilted Sun-Facing
Surface (Dotted Line) Computed Using Smarts Version 2.9.2 Model With
Input File in
    FIG. 1 Plot of Direct Normal Spectral Irradiance (Solid Line) and Hemispherical Spectral Irradiance on 37° Tilted Sun-Facing Surface (Dotted Line) Computed Using Smarts Version 2.9.2 Model With Input File in Table 1
    TABLE 1 SMARTS Version 2.9.2 Input File to Generate the Reference Spectra

    Card ID


    Parameter/Description/Variable Name


    'ASTM_G 173_Std_Spectra'




    Pressure input mode (1 = pressure and altitude): ISPR


    1013.25 0.

    Station Pressure (mb) and altitude (km): SPR, ALT



    Standard Atmosphere Profile Selection (1 = use default atmosphere): IATM1



    Default Standard Atmosphere Profile: ATM



    Water Vapor Input (1 = default from Atmospheric Profile): IH2O



    Ozone Calculation (1 = default from Atmospheric Profile): IO3



    Pollution level mode (1 = standard conditions/no pollution): IGAS (see X1.3)



    Carbon Dioxide volume mixing ratio (ppm): qCO2 (see X1.3)



    Extraterrestrial Spectrum (1 = SMARTS/Gueymard): ISPCTR



    Aerosol Profile to Use: AEROS



    Specification for aerosol optical depth/turbidity input (0 = AOD at 500 nm): ITURB



    Aerosol Optical Depth at 500 nm: TAU5



    Far field Spectral Albedo file to use (38= Light Sandy Soil): IALBDX



    Specify tilt calculation (1 = yes): ITILT


    38 37 180

    Albedo and Tilt variables-Albedo file to use for near field, Tilt, and Azimuth: IALBDG, TILT, WAZIM


    280 4000 1.0 1367.0

    Wavelength Range-start, stop, mean radius vector correction, integrated solar spectrum irradiance: WLMN, WLMX, SUNCOR, SOLARC



    Separate spectral output file print mode (2 = yes): IPRT


    280 4000 .5

    Output file wavelength-Print limits, start, stop, minimum step size: WPMN, WPMX, INTVL



    Number of output variables to print: IOTOT


    8 9

    Code relating output variables to print (8 = Hemispherical tilt, 9 = direct normal + circumsolar): OUT(8), OUT(9)



    Circumsolar calculation mode (1 = yes): ICIRC


    0 2.9 0

    Receiver geometry-Slope, View, Limit half angles: SLOPE, APERT, LIMIT



    Smooth function mode (0 = none): ISCAN



    Illuminance calculation mode (0 = none): ILLUM



    UV calculation mode (0 = none): IUV



    Solar Geometry mode (2 = Air Mass): IMASS



    Air mass value: AMASS

    4.6 The availability of the adjunct (ADJG173CD3) standard computer software for SMARTS allows one to (1) reproduce the reference spectra, using the above input parameters; (2) compute test spectra to attempt to match measured data at a specified FWHM, and evaluate atmospheric conditions; and (3) compute test spectra representing specific conditions for analysis vis-à-vis any one or all of the reference spectra.

    4.7 Differences from the previous standard spectra (G159) can be summarized as follows:

    4.7.1 Extended spectral interval in the ultraviolet (down to 280 nm, rather than 305 nm),

    4.7.2 Better resolution (2002 wavelengths, as compared to 120),

    4.7.3 Constant intervals (0.5 nm below 400 nm, 1 nm between 400 and 1700 nm, and 5 nm above),

    4.7.4 Better definition of atmospheric scattering and gaseous absorption, with more species considered,

    4.7.5 Better defined extraterrestrial spectrum,

    4.7.6 More realistic spectral ground reflectance, and

    4.7.7 Lower aerosol optical depth, yielding significantly larger direct normal irradiance.

    1. Scope

    1.1 These tables contain terrestrial solar spectral irradiance distributions for use in terrestrial applications that require a standard reference spectral irradiance for hemispherical solar irradiance (consisting of both direct and diffuse components) incident on a sun-facing, 37° tilted surface or the direct normal spectral irradiance. The data contained in these tables reflect reference spectra with uniform wavelength interval (0.5 nanometer (nm) below 400 nm, 1 nm between 400 and 1700 nm, an intermediate wavelength at 1702 nm, and 5 nm intervals from 1705 to 4000 nm). The data tables represent reasonable cloudless atmospheric conditions favorable for photovoltaic (PV) energy production, as well as weathering and durability exposure applications.

    1.2 The 37° slope of the sun-facing tilted surface was chosen to represent the average latitude of the 48 contiguous United States. A wide variety of orientations is possible for exposed surfaces. The availability of the SMARTS model (as an adjunct, ADJG173CD3) to this standard) used to generate the standard spectra allows users to evaluate differences relative to the surface specified here.

    1.3 The air mass and atmospheric extinction parameters are chosen to provide (1) historical continuity with respect to previous standard spectra, ( 2) reasonable cloudless atmospheric conditions favorable for photovoltaic (PV) energy production or weathering and durability exposure, based upon modern broadband solar radiation data, atmospheric profiles, and improved knowledge of aerosol optical depth profiles. In nature, an extremely large range of atmospheric conditions can be encountered even under cloudless skies. Considerable departure from the reference spectra may be observed depending on time of day, geographical location, and changing atmospheric conditions. The availability of the SMARTS model (as an adjunct (ADJG173CD3)to this standard) used to generate the standard spectra allows users to evaluate spectral differences relative to the spectra specified here.

    2. Referenced Documents (purchase separately) The documents listed below are referenced within the subject standard but are not provided as part of the standard.

    ASTM Standards

    E490 Standard Solar Constant and Zero Air Mass Solar Spectral Irradiance Tables

    E772 Terminology of Solar Energy Conversion

    ICS Code

    ICS Number Code 17.180.01 (Optics and optical measurement in general)

    UNSPSC Code

    UNSPSC Code

    Referencing This Standard
    Link Here
    Link to Active (This link will always route to the current Active version of the standard.)

    DOI: 10.1520/G0173-03R12

    Citation Format

    ASTM G173-03(2012), Standard Tables for Reference Solar Spectral Irradiances: Direct Normal and Hemispherical on 37° Tilted Surface, ASTM International, West Conshohocken, PA, 2012,

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