| 1. | Window radiation is radiation that actually passes through the atmospheric window.
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| 2. | Non-window radiation is radiation that actually does not pass through the atmospheric window.
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| 3. | Atmospheric windows in the infrared spectrum are also employed to perform chemical imaging remotely.
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| 4. | Bonds to other halogens also absorb in the atmospheric window, though much less strongly.
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| 5. | Thus, the existence of an atmospheric window is critical to Earth remaining a habitable planet.
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| 6. | There is, however, still the problem of the C-F bonds absorbing in the atmospheric window.
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| 7. | The infrared atmospheric window is a path from the land-sea surface of the earth to space.
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| 8. | These regions are called atmospheric windows.
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| 9. | Non-window wavelength radiation is radiation that, judging only from its wavelength, is unlikely to pass through the atmospheric window.
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| 10. | In the atmospheric window between approximately 8000 and 14000 nm, in the far-infrared spectrum, carbon dioxide and water absorption is weak.
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