Optical window

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Rough plot of Earth's atmospheric transmittance (or opacity) to various wavelengths of electromagnetic radiation, including visible light.

The optical window is the portion of the optical spectrum that is Template:Em blocked by the Earth's atmosphere. The window runs from around 300 nanometers (ultraviolet-B) up into the range the human eye can detect, roughly 400–700 nm and continues up to approximately 2 μm.<ref>Template:Cite book</ref><ref>Template:Cite book</ref> Sunlight mostly reaches the ground through the optical atmospheric window;<ref name=":1">Template:Cite book</ref><ref>Template:Cite book</ref> the Sun is particularly active in most of this range (44% of the radiation emitted by the Sun falls within the visible spectrum and 49% falls within the infrared spectrum).<ref>Template:Cite web</ref>

Definition

The Earth's atmosphere is not totally transparent and is in fact 100% opaque to many wavelengths (see plot of Earth's opacity); the wavelength ranges to which it is transparent are called atmospheric windows.<ref>Template:Cite web</ref>

Disambiguation of the term 'optical spectrum'

Although the word optical, deriving from Ancient Greek ὀπτῐκός (optikós, "of or for sight"), generally refers to something visible or visual,<ref>Template:Cite web</ref> the term optical spectrum is used to describe the sum of the visible, the ultraviolet and the infrared spectra (at least in this context).<ref>Template:Cite book</ref><ref>Template:Cite book</ref>

Optical atmospheric window

Solar irradiance spectrum above atmosphere and at surface. Extreme UV and X-rays are produced (at left of wavelength range shown) but comprise very small amounts of the Sun's total output power.

The optical atmospheric window is the optical portion of the electromagnetic spectrum that passes through the Earth's atmosphere, excluding its infrared part;<ref>Template:Cite book</ref> although, as mentioned before, the optical spectrum also includes the IR spectrum and thus the optical window could include the infrared window (8 – 14 μm), the latter is considered separate by convention, since the visible spectrum is not contained in it.<ref>Template:Cite book</ref>

Historical importance for observational astronomy

Up until the 1940s, astronomers could only use the visible and near infrared portions of the optical spectrum for their observations. The first great astronomical discoveries such as the ones made by the famous Italian polymath Galileo Galilei were made using optical telescopes that received light reaching the ground through the optical window.<ref>Template:Cite book</ref> After the 1940s, the development of radio telescopes gave rise to the even more successful field of radio astronomy that utilized the radio window.<ref>Template:Cite book</ref>

See also

References

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