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Introduction to solar energy/Equations

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Solar resources and availability

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TST=UTC+longitude15+EoT

Precise method

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EoT=Δtey=−7.659sin⁡(D)+9.863sin⁡(2D+3.5932)(minutes)

where: D=6.24004077+0.01720197(365.25(y−2000)+d)

where d represents the number of days since 1 January of the current year, y.

Rough approximation

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For EoT in minutes, see the following equation. Ensure that the trigonometry relations are calculated in radians mode.

EoT(minutes)=Δtey=7.678sin⁡(B+1.374)−9.87sin⁡(2B)

Where B is:

B=2π(n−81)365

Where n is the day of the year.

For EoT in degrees, see the following equation. Ensure that the trigonometry relations are calculated in degrees mode.

EoT(degrees)=0.0072cos(J)−0.0528cos(2J)−0.0012cos(3J)−0.1229sin(J)−0.1565sin(2J)−0.0041sin(3J)Where J is:

J=n×360365

Where n is the day of the year.

Solar declination rough approximation, in degrees

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δdegrees=23.45sin(360(n+284)/365)

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Solar declination finer result, in radians

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δradians=arcsin(0.369sin(360(n−82)/365+2sin(360(n−2)/365))

Solar declination finer result, in degrees

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δradians=0.33281−22.984cos(J)−0.3499cos(2J)−0.1398cos(3J)+3.7872sin(J)+0.03205sin(2J)+0.07187(3J0

Where J is the day of the year, with January 1st being n=1.

J=n×(360/365), in degrees.

Half hour angle, ω₀

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Calculate the hour angle when the altitude angle is equal to 0.

ω0(degrees)=arccos(−(tan⁡δ)∗(tan⁡Lat))

Using this equation, you can find true solar time (TST) at sunrise and at sunset.

TSTsunrise=12−(115)ω0, make sure that ω0is in degrees.

TSTsunset=12+(115)ω0, make sure that ω0is in degrees.

S0=(215)ω0, make sure that ω0is in degrees.

if: ω0>90, then the day is longer than the night, and the time that the sun is in the sky is at least 12 hours.

if: ω0<90, then the day is shorter than the night, and the time that the sun is in the sky is less than 12 hours.

Elevation angle, h

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h=arcsin[cos(δ−Lat)]=90∘−Lat+δ

h=arcsin(cos⁡δcos⁡HAcos⁡Lat+sin⁡δsin⁡Lat)