{"id":1775,"date":"2024-10-11T10:06:32","date_gmt":"2024-10-11T09:06:32","guid":{"rendered":"http:\/\/guemisa.es\/?post_type=documentos-pdf&#038;p=1775"},"modified":"2026-11-03T13:42:35","modified_gmt":"2026-11-03T12:42:35","slug":"magnitudes-of-solar-radiation","status":"publish","type":"documentos-pdf","link":"https:\/\/guemisa.es\/en\/documentos-pdf\/magnitudes-radiacion-solar\/","title":{"rendered":"Measurement of solar radiation: magnitudes, pyranometers and pyrheliometers"},"content":{"rendered":"<div class=\"gm-doc gm-m-guemisa\">\n<p class=\"k\">Technical tutorial \u00b7 GUEMISA<\/p>\n<div class=\"meta\"><span>Irradiance W m-2<\/span><span>Pyranometer<\/span><span>Pyrheliometer<\/span><span>Direct, diffuse and global radiation<\/span><span>Heliograph<\/span><\/div>\n<div class=\"resp\"><b class=\"t\">Quick response<\/b>Global solar radiation is the sum of the radiation <b>direct, diffuse and reflected<\/b>. It is measured with pyranometers (global and diffuse, spectral range of 0.3 to 3.0 \u03bcm) and pyrheliometers (direct, on solar tracker); the recommended unit of irradiance is <b>W m<sup>-2<\/sup><\/b>.<\/div>\n<h2>Magnitudes of solar radiation<\/h2>\n<div class=\"tw\"><table><thead><tr><th>Magnitude<\/th><th>Definition<\/th><th>How is it measured?<\/th><\/tr><\/thead><tbody><tr><td>Direct radiation<\/td><td>It comes directly from the solar disk.<\/td><td>With systems to track the movement of the Sun<\/td><\/tr><tr><td>Diffuse radiation<\/td><td>It comes from reflections in the atmosphere<\/td><td>With solar disk shading systems<\/td><\/tr><tr><td>Reflected radiation<\/td><td>Radiation reflected by the surroundings of the receiving surface that strikes an inclined surface; its average value is 20% of the global radiation on a horizontal surface<\/td><td>It is not usually measured<\/td><\/tr><tr><td>Global radiation<\/td><td>Sum of direct, diffuse and reflected radiation received per unit area<\/td><td>It is usually measured on a horizontal surface; sometimes in the arrangement of the panels<\/td><\/tr><\/tbody><\/table><\/div>\n<p>95% of extraterrestrial solar radiation is between 0.2 and 3 \u03bcm. Terrestrial radiation is longwave: at 300 K, 99.99 percent of its energy has a wavelength greater than 3 \u03bcm.<\/p>\n<h2>Units and spectrum<\/h2>\n<div class=\"tw\"><table><thead><tr><th>Magnitude<\/th><th>Recommended unit<\/th><\/tr><\/thead><tbody><tr><td>Irradiance (power)<\/td><td>watts per square meter (W m <sup>-2<\/sup> )<\/td><\/tr><tr><td>Radiant exposure (energy)<\/td><td>joules per square meter (J m <sup>-2<\/sup> )<\/td><\/tr><tr><td>Spectral irradiance<\/td><td>W m <sup>-2<\/sup> nm <sup>-1<\/sup><\/td><\/tr><tr><td>Spectral radiant exposure<\/td><td>J m <sup>-2<\/sup> nm <sup>-1<\/sup><\/td><\/tr><\/tbody><\/table><\/div>\n<div class=\"tw\"><table><thead><tr><th>Band<\/th><th>Interval<\/th><\/tr><\/thead><tbody><tr><td>Visible light (99% of visible radiation)<\/td><td>400 nm to 730 nm<\/td><\/tr><tr><td>GRAPE<\/td><td>315 to 400 nm<\/td><\/tr><tr><td>UV-B<\/td><td>280 to 315 nm<\/td><\/tr><tr><td>UV-C<\/td><td>100 to 280 nm<\/td><\/tr><tr><td>Shortwave extraterrestrial solar radiation (97%)<\/td><td>0.29 \u03bcm to 3.00 \u03bcm<\/td><\/tr><\/tbody><\/table><\/div>\n<h2>Accuracy, precision, and integration period<\/h2>\n<p>Accuracy expresses the uncertainty in the agreement between the measured value and the true value. The precision of the instrument is determined by:<\/p>\n<ul><li>Resolution: the smallest variation of radiation that it can detect.<\/li><li>Variations in sensitivity due to alterations in environmental variables.<\/li><li>The non-linearity of the response.<\/li><li>The deviation of the spectral response from the postulated one.<\/li><li>The deviation of the directional response (cosine and azimuthal).<\/li><\/ul>\n<p>It is recommended to record data at a frequency one order of magnitude higher than required: hourly data if daily data is required, and minutely data if hourly data is required.<\/p>\n<h2>Pyrheliometers and direct radiation<\/h2>\n<p>The pyrheliometer measures direct solar radiation with its receiving surface oriented perpendicular to the incident rays. It includes a shutter to measure only the radiation from the Sun and a very close ring-shaped region of the sky. In modern instruments, this covers a half-angle of approximately 2.5\u00b0; in older instruments, it was about 8\u00b0.<\/p>\n<div class=\"tw\"><table><thead><tr><th>Guy<\/th><th>Characteristics<\/th><\/tr><\/thead><tbody><tr><td>Primary (absolute) pattern<\/td><td>Defines the total irradiance scale without resorting to reference sources; electrically calibrated cavity receivers and differential heat flux meters<\/td><\/tr><tr><td>Secondary pattern<\/td><td>\u00c5ngstr\u00f6m compensation and silver disc; they are calibrated by comparison with a primary standard.<\/td><\/tr><tr><td>First and second class<\/td><td>Thermopile detectors; continuous recording; annual accuracy greater than one percent (first class) and two percent (second class); maximum response time of ten seconds (first class) and thirty seconds (second class)<\/td><\/tr><\/tbody><\/table><\/div>\n<p>Measuring direct radiation requires orientation perpendicular to the sun's rays, which is achieved with solar trackers. When choosing a tracker, factors to consider include tracking accuracy, clock accuracy, weight capacity, and compatible devices.<\/p>\n<h2>Pyranometers: global and diffuse radiation<\/h2>\n<p>The pyranometer measures solar radiation from an angle of 2\u03c0 steradians onto a flat surface, within a spectral range of 0.3 to 3.0 \u03bcm. It is mounted in an inverted position to measure the global reflected radiation. For diffuse radiation, the direct component is covered with a screen or shade band.<\/p>\n<div class=\"tw\"><table><thead><tr><th>Feature<\/th><th>Secondary pattern<\/th><th>First class<\/th><th>Second class<\/th><\/tr><\/thead><tbody><tr><td>Resolution (minimum detectable variation in W m <sup>-2<\/sup> )<\/td><td>\u00b1 1<\/td><td>\u00b1 5<\/td><td>\u00b1 10<\/td><\/tr><tr><td>Stability (% of full scale, variation\/year)<\/td><td>\u00b1 1<\/td><td>\u00b1 2<\/td><td>\u00b1 5<\/td><\/tr><tr><td>Cosine response (% deviation for solar altitude of 10\u00ba)<\/td><td>&lt;\u00b1 3<\/td><td>&lt;\u00b1 7<\/td><td>&lt;\u00b1 15<\/td><\/tr><tr><td>Azimuthal response (% deviation for a solar altitude of 10\u00ba)<\/td><td>&lt;\u00b1 3<\/td><td>&lt;\u00b1 5<\/td><td>&lt;\u00b1 10<\/td><\/tr><tr><td>Temperature response (maximum % error)<\/td><td>\u00b1 1<\/td><td>\u00b1 2<\/td><td>\u00b1 5<\/td><\/tr><tr><td>Nonlinearity (% of full scale)<\/td><td>\u00b1 0.5<\/td><td>\u00b1 2<\/td><td>\u00b1 5<\/td><\/tr><tr><td>Spectral sensitivity (% deviation, 0.3 to 3 \u03bcm)<\/td><td>\u00b1 2<\/td><td>\u00b1 5<\/td><td>\u00b1 10<\/td><\/tr><tr><td>Response time (99% response rate)<\/td><td>&lt;25 s<\/td><td>&lt;1 min<\/td><td>&lt;4 min<\/td><\/tr><\/tbody><\/table><\/div>\n<div class=\"figs\"><figure><a href=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p10-2.png\" target=\"_blank\" rel=\"noopener\"><img decoding=\"async\" src=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p10-2.png\" alt=\"Pyranometer with shadow band for measuring diffuse radiation\" loading=\"lazy\"><\/a><figcaption>Pyranometer with shadow band for measuring diffuse radiation<\/figcaption><\/figure><figure><a href=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p11-1.png\" target=\"_blank\" rel=\"noopener\"><img decoding=\"async\" src=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p11-1.png\" alt=\"Solar tracker with instruments for direct, diffuse and infrared radiation\" loading=\"lazy\"><\/a><figcaption>Solar tracker with instruments for direct, diffuse and infrared radiation<\/figcaption><\/figure><\/div>\n<h2>Hours of sunlight, spectrum, and data acquisition<\/h2>\n<p>The hours of sunshine are recorded with the Campbell Stokes heliograph: a solid glass ball approximately 96 mm in diameter and a concentric metal cap into which a strip of cardboard with hourly divisions is inserted each day; the sun burns footprints according to the intensity of its rays.<\/p>\n<figure><a href=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p12-1.png\" target=\"_blank\" rel=\"noopener\"><img decoding=\"async\" src=\"https:\/\/guemisa.es\/wp-content\/uploads\/2026\/11\/magnitudes-radiacion-solar-figura-p12-1.png\" alt=\"Heliograph\" loading=\"lazy\"><\/a><figcaption>Heliograph<\/figcaption><\/figure>\n<p>The spectral distribution is measured using spectroradiometers. The sensor signals are stored in a datalogger connected to a PC via serial cable, telephone network (MODEM), or the internet if the equipment allows an IP address.<\/p>\n<h2>Frequently Asked Questions<\/h2><details class=\"faq\"><summary>What is global solar radiation?<\/summary><p>Solar radiation received per unit area: sum of the direct, diffuse and reflected components.<\/p><\/details><details class=\"faq\"><summary>What instrument is used to measure direct radiation?<\/summary><p>With a pyrheliometer mounted on a solar tracker.<\/p><\/details><details class=\"faq\"><summary>What does a pyranometer measure?<\/summary><p>Solar radiation from an angle of 2\u03c0 steradians on a flat surface, in the range of 0.3 to 3.0 \u03bcm.<\/p><\/details><details class=\"faq\"><summary>What unit is recommended for irradiance?<\/summary><p>Watts per square meter (W m-2); for radiant exposure, joules per square meter (J m-2).<\/p><\/details><details class=\"faq\"><summary>How is diffuse radiation measured?<\/summary><p>With shading devices: shade bands or solar trackers with point shading of the Sun.<\/p><\/details><details class=\"faq\"><summary>What recording frequency is recommended?<\/summary><p>An order of magnitude greater than required: hourly data for daily requirements and minute data for hourly requirements.<\/p><\/details>\n<h2>Related<\/h2><ul class=\"rel\"><li><a href=\"https:\/\/guemisa.es\/en\/category\/weather-sensors\/\">Weather sensors<\/a><\/li><li><a href=\"https:\/\/guemisa.es\/en\/category\/solar-radiation-light\/\">Solar radiation \u2013 Light<\/a><\/li><li><a href=\"https:\/\/guemisa.es\/en\/pdf-documents\/beaufort-wind-scale\/\">Beaufort wind scale<\/a><\/li><li><a href=\"https:\/\/guemisa.es\/en\/category\/data-logger\/\">Data Logger<\/a><\/li><li><a href=\"https:\/\/guemisa.es\/en\/pdf-documents\/solar-wind-sector-sensor-sheet\/\">TST-1x and YCA360 inclinometers for solar and wind energy<\/a><\/li><li><a href=\"https:\/\/guemisa.es\/en\/technical-information\/\">All technical information about GUEMISA<\/a><\/li><\/ul>\n<p class=\"pdf-fin\">Below, the original PDF document is available for viewing or downloading.<\/p><\/div>","protected":false},"featured_media":14179,"template":"","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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