Cosine of solar zenith angle.
The solar constant is measured at what altitude.
The interaction of the solar wind and upper layers of earth s atmosphere.
Global and direct uv irradiance spectra were measured under a cloudless sky at varying solar elevations at inns bruck 577 m a s l and hafelekar 2300 m a s l from january to march 1992.
Multiply your uncorrected solar irradiation by 2 to correct for the glass and also by 1 4 to correct for the atmosphere.
It is measured by satellite as being 1 361 kilowatts per square meter at solar minimum and approximately 0 1 greater at solar maximum.
The value of the constant is approximately 1 366 kilowatts per square metre.
Energy in the ultraviolet and visible regions for λ less than 607 nanometers was 7 0 percent.
Must be measured at aphelion.
Must be measured at perihelion.
The solar constant is not a physical constant in the modern codat.
Earth s solar constant a.
The solar constant is a flux density measuring mean solar electromagnetic radiation per unit area.
Refers to the intensity of solar radiation that actually reaches earth s surface.
The solar constant was directly measured from an altitude of about 82 kilometers apparently the first such determination.
Az el both report dark after astronomical twilight.
Is about 0 5 calories per square centimeter per minute.
The total solar intensity was 136 1 milliwatts per square centimeter or 1 952 calories per square centimeter per minute about 2 5 percent less than johnson s derived value.
The sun s altitude refers to.
The solar constant is measured at.
Then your difference is.
Solar constant irradiation 2 1 4 j s m2 the accepted value of the solar constant is about 1376 w m2.
Elevation is measured in degrees up from the horizon.
Solar constant the total radiation energy received from the sun per unit of time per unit of area on a theoretical surface perpendicular to the sun s rays and at earth s mean distance from the sun.
Your solar constant 1376 1376 100 include your sign.
It is most accurately measured from satellites where atmospheric effects are absent.
The solar constant has been measured by the use of eppley normal incidence pyrhelio meters on three different days at 31 kilometers altitude.
It is measured on a surface perpendicular to the rays one astronomical unit from the sun.
After correcting the readings for the remaining 1 of the atmosphere and earth sun distance a value of 1 912 gm cal cm 2 min has been determined for the solar constant.
The spectra were measured with the bentham spectrometer.