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SUN RADIATION

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An equation describe the variation through out the year just outside the<br />

earth atmosphere:<br />

H<br />

H<br />

const<br />

=<br />

1<br />

+<br />

0.<br />

033<br />

cos(<br />

360<br />

( n<br />

365<br />

where:<br />

H is the radiant power density outside the Earth's atmosphere (in W/m2);<br />

H const is the value of the solar constant, 1.353 kW/m2; and<br />

n is the day of the year.<br />

−<br />

2)<br />

MAGISTER TEKNIK ELEKTRO<br />

)

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