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Direct Energy, 2018a

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6 PHOTOVOLTAICS 127<br />

Figure 6.14: Diagram of atmospheric windows wavelengths at which electromagnetic<br />

radiation will penetrate the Earth's atmosphere. Chemical<br />

Notation (CO 2 ,O 3 ) indicates the gas responsible for blocking sunlight at<br />

a particular wavelength. This gure is used with permission [72].<br />

energy cannot.<br />

If a temperature gradient is applied across a pn junction, charges ow.<br />

When one side of the device is heated, charges move more rapidly and these<br />

energetic charges diuse to the cooler side. This eect, called the Seebeck<br />

thermoelectric eect, is discussed in Chapter 8.<br />

6.6 Solar Cells<br />

6.6.1 Solar Cell Eciency<br />

<strong>Energy</strong> conversion devices are never 100% ecient. Eciency is dened as<br />

the output power over the input power. Eciency of a solar cell is often<br />

dened as the ratio of electrical power out to optical power in to the device.<br />

η eff = P electrical out<br />

P optical in<br />

(6.23)<br />

Not all sunlight reaches a solar cell because some of it is absorbed by<br />

the earth's atmosphere. This atmospheric absorption is strongly dependent<br />

on wavelength. Figure 6.14 is a plot of the transmissivity of the<br />

atmosphere as a function of wavelength. It plots the percent of light which<br />

passes through the atmosphere without getting absorbed. Some gases in<br />

the atmosphere, such as water vapor and CO 2 , absorb a signicant amount<br />

of energy at particular wavelengths. The gure indicates which gas is responsible<br />

for atmospheric absorption at some particular wavelengths. For<br />

example, ozone O 3 absorbs ultraviolet light. Ozone in the atmosphere oers<br />

benets because ultraviolet light can damage eyes and skin. The intensity<br />

of the optical power from the sun that is hits a solar cell varies from day

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