c1 drafted · lead Global horizontal irradiance
DNI, GHI and diffuse horizontal irradiation together usually define a site's solar resource.
- Utility Scale Power Plants - A Guide for Investors and Developers
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Direct normal irradiance is the solar power received per unit area on a surface that always faces the sun directly. When it is summed over a period as energy, it is called direct normal irradiation. Direct normal irradiation, global horizontal irradiation and diffuse horizontal irradiation are the values normally used to describe the solar resource at a site. DNI matters most for systems that track the sun and for concentrating technologies, because concentrating technologies can only use the direct beam. The irradiance on a PV array is the sum of three components: direct beam, diffuse sky and albedo. DNI is measured with a pyrheliometer. The beam irradiance on the module plane is DNI multiplied by the cosine of the angle of incidence. Weather stations and data loggers often report DNI as a separate data point in watts per square meter. During irradiance transposition, software subtracts the estimated diffuse part and re-angles the remaining direct beam to the module orientation. It then adds the diffuse part back. When the sun is very low, it assumes there is no direct beam.
related_toc1 drafted · lead Global horizontal irradiance
DNI, GHI and diffuse horizontal irradiation together usually define a site's solar resource.
sec=3.1 h=f07096ada173c2 verified · fact Diffuse horizontal irradiance
The beam and diffuse components are measured separately in the detailed laboratory approach.
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c3 drafted · lead Plane-of-array irradiance
Plane-of-array irradiance is the sum of the direct beam, diffuse sky and albedo components.
sec=front h=0dbda907089fsec=h3 h=ab5e834dc829sec=front h=53994d8c99ffreview note: support check: partial - POA is stated as the sum of direct, diffuse and albedo components, but the passages do not explicitly link DNI itself to POA (direct beam is not named as DNI).
c4 drafted · lead Irradiance transposition
During transposition, trigonometry is applied to the direct beam part only, after the estimated diffuse part has been removed.
sec=front h=0dbda907089fsec=front h=429855123554review note: support check: partial - The transposition process is described as subtracting diffuse and applying trigonometry to the direct beam, but it is applied to direct horizontal irradiance, not explicitly DNI.
c5 drafted · lead Clear-sky irradiance model
Clear-sky direct and diffuse irradiance are calculated from the time of day, latitude and longitude.
sec=front h=0dbda907089fsec=front h=429855123554review note: support check: partial - Clear-sky direct and diffuse horizontal irradiance are computed from time, latitude, longitude, but the link to DNI specifically is not stated.
Albedo is the third component of surface irradiance, alongside the direct and diffuse components.
sec=front h=0dbda907089fsec=h3 h=ab5e834dc829review note: support check: partial - Albedo is stated as the third component alongside direct and diffuse, but no relation to DNI is stated.
c7 drafted · lead Pyrheliometer proposed
DNI is measured with a thermopile pyrheliometer, also called a normal incidence pyrheliometer.
sec=h30 h=67b7cdd52848tbl=4.r27 h=aab301c47224review note: support check: partial - DNI is from a pyrheliometer and a 'normal incidence pyrheliometer' entry exists, but 'thermopile' and 'also called' are only loosely supported.
In the Sandia model, an air mass spectral function is applied together with the beam irradiance.
sec=h30 h=67b7cdd52848review note: support check: partial - The Sandia equation applies an air mass function f1(AMa) with Eb, but it multiplies the whole bracket rather than only the beam term, and the relation to DNI is only indirect.
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