03-30-2015, 01:38 PM
From my blog: http://edspi31415.blogspot.com/2015/03/h...solar.html
Solar Irradiance
The program IRRAD will calculate two properties:
(1) The solar angle of incidence given the angular elevation and azimuth (from south going “counterclockwise”: east-north-west) of both the sun and panel.
(2) The irradiance given by the solar panel.
Formulas
Angle of Incidence Given Azimuth
Degree mode is assumed, the angle of incidence (θ) is found in the following equation:
cos θ = cos(ep)*sin(es) + sin(ep)*cos(es)*cos(as-ap)
Where:
θ = angle of incidence
es = elevation of the sun
ep = elevation of the panel
as = azimuth of the sun, from south headed towards east, then north, then west
ap = azimuth of the panel, from south headed towards east, then north, then west
Calculating Flux Density of Solar Radiation on a Surface
Calculating the flux density (energy) of solar radiation on a surface, Lambert’s Cosine Law is used. Lambert’s Cosine Law states that the relation between the irradiance of the sun and the angle of incidence. The result is the irradiance of the surface. Irradiance is the rate of energy (power) over a unit area. In SI units, irradiance is measured in Watts per square meter (W/m^2).
ls = lb * cos θ
Where:
lb = the sun’s power or irradiance. Often this is treated as a constant, which is approximately 1367 W/m^2 for extraterrestrial solar power, or approximately 1000 W/m^2 when we are dealing with the Earth’s surface (taking scattering of light into account)
ls = the panel’s power or irradiance
Program IRRAD:
Data:
Sun:
Elevation: 55⁰24’21” ≈ 55.40583⁰
Azimuth: 175⁰15’44” ≈ 175.26222⁰
Panel:
Elevation: 40⁰
Azimuth: 90⁰ (panel is facing due east)
Irradiance of the Sun: 1000 W/m^2
Output:
Incidence Angle ≈ 48.643169⁰
Surface Radiance ≈ 660.746510 W/m^2
Sources:
Baldocchi, Dennis “Lecture 7, Solar Radiation, Part 3, Earth-Sun Geometry” Biometeorogy, ESPM 129 University of California, Berkeley.
http://nature.berkeley.edu/biometlab/esp...0notes.pdf
Retrieved February 17, 2015.
Mortimer, David “Lambert’s Cosine Law” 30 January 2014. The Solar Bucket.
http://thesolarbucket.blogspot.com/2014/...e-law.html
Retrieved March 18, 2015
University of Oregon Solar Radiation Monitoring Laboratory “Solar Radiation Basics” University of Oregon. http://solardat.uoregon.edu/SolarRadiationBasics.html Retrieved February 10, 2015
Solar Irradiance
The program IRRAD will calculate two properties:
(1) The solar angle of incidence given the angular elevation and azimuth (from south going “counterclockwise”: east-north-west) of both the sun and panel.
(2) The irradiance given by the solar panel.
Formulas
Angle of Incidence Given Azimuth
Degree mode is assumed, the angle of incidence (θ) is found in the following equation:
cos θ = cos(ep)*sin(es) + sin(ep)*cos(es)*cos(as-ap)
Where:
θ = angle of incidence
es = elevation of the sun
ep = elevation of the panel
as = azimuth of the sun, from south headed towards east, then north, then west
ap = azimuth of the panel, from south headed towards east, then north, then west
Calculating Flux Density of Solar Radiation on a Surface
Calculating the flux density (energy) of solar radiation on a surface, Lambert’s Cosine Law is used. Lambert’s Cosine Law states that the relation between the irradiance of the sun and the angle of incidence. The result is the irradiance of the surface. Irradiance is the rate of energy (power) over a unit area. In SI units, irradiance is measured in Watts per square meter (W/m^2).
ls = lb * cos θ
Where:
lb = the sun’s power or irradiance. Often this is treated as a constant, which is approximately 1367 W/m^2 for extraterrestrial solar power, or approximately 1000 W/m^2 when we are dealing with the Earth’s surface (taking scattering of light into account)
ls = the panel’s power or irradiance
Program IRRAD:
Code:
EXPORT IRRAD()
BEGIN
LOCAL es,as,ep,ap,θinc;
LOCAL ib,is;
HAngle:=1;
INPUT({es,as},”Sun”,{“Elev.:”,”Azi (S):”});
INPUT({ep,ap},”Panel”,{“Elev.:”,”Azi (S):”});
INPUT(ib,”Sun’s Irradiance”,”I:”,”W/m^2”);
// angle of incidence
θinc:=ACOS(COS(ep)*SIN(es)+SIN(ep)*COS(es)*COS(as-ap));
MSGBOX(“Incidence Angle = “+θinc);
// Lambert’s Cosine Law
Is:=ib*COS(θinc);
MSGBOX(“Surface Irradiance = “+is);
RETURN {θinc,is};
END;
Data:
Sun:
Elevation: 55⁰24’21” ≈ 55.40583⁰
Azimuth: 175⁰15’44” ≈ 175.26222⁰
Panel:
Elevation: 40⁰
Azimuth: 90⁰ (panel is facing due east)
Irradiance of the Sun: 1000 W/m^2
Output:
Incidence Angle ≈ 48.643169⁰
Surface Radiance ≈ 660.746510 W/m^2
Sources:
Baldocchi, Dennis “Lecture 7, Solar Radiation, Part 3, Earth-Sun Geometry” Biometeorogy, ESPM 129 University of California, Berkeley.
http://nature.berkeley.edu/biometlab/esp...0notes.pdf
Retrieved February 17, 2015.
Mortimer, David “Lambert’s Cosine Law” 30 January 2014. The Solar Bucket.
http://thesolarbucket.blogspot.com/2014/...e-law.html
Retrieved March 18, 2015
University of Oregon Solar Radiation Monitoring Laboratory “Solar Radiation Basics” University of Oregon. http://solardat.uoregon.edu/SolarRadiationBasics.html Retrieved February 10, 2015