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Pyrgeometer physical properties, Spectral range – Kipp&Zonen CGR 4 Pyrgeometers User Manual

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4. Pyrgeometer physical properties

4.1. Spectral range

The spectral properties of the pyrgeometer are mainly determined by the filter characteristics of the silicon

window and the coatings. The application is primarily to measure long-wave downward atmospheric

radiation. The spectral range is from 4.5 to 42 µm, where most of this radiation is present.

Figure 11:

Pyrgeometer spectral window properties

The atmosphere is transparent to long-wave radiation emitted by the Earth’s surface in certain wavelength

intervals, particularly within a spectral range of approximately 8 to 14 µm. This is called the ‘atmospheric

window’. Within this spectral range the Earth is able to maintain an equilibrium temperature by losing a

certain quantity of heat gained each day from the sun.

The sun radiates approximately as a blackbody at an equivalent temperature of 5770K. Almost 99% of its

emitted energy is contained in wavelengths less than 4µm, called short-wave radiation. The equivalent

radiant temperature of the Earth’s surface is about 275K. More than 99% of this energy is emitted at

wavelengths greater than 3 µm and is called long-wave, thermal, or infrared radiation.

Downward long-wave radiation is a result of atmospheric

re-emission. Re-emission is the reversible effect of

absorption of long-wave radiation emitted by the Earth

and by chemical elements such as water (H₂O), Oxygen

(O₂), Ozone (O₃), Carbon dioxide (CO₂), etc. These

elements are the main emitters of long-wave radiation in

the atmosphere. The remaining unabsorbed portion of the

Earth’s radiation escapes into outer space. Under clear skies

an object can be cooled below ambient air temperature by

radiative heat loss to the sky.

Observing the earth from outer space, a blackbody is seen

in a range of 8 to 14 µm with a temperature of 14°C and

outside this wavelength range a blackbody of -60°C.

Under clear sky conditions in a reverse direction, outer Figure 12: Atmospheric radiation

space can be observed in the same spectral range.

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CGR 4 Manual