File:SpectroscopyResearch 021.jpg

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Description Because the distance of Mars was decreasing at the time, there is a Doppler shift in the Martian spectrum towards the shorter wavelengths. However, this only affects lines originating on Mars or present in the original sunlight that Mars reflects. The Doppler shift is clearly eviden at places marked by arrows. In the case of the strong absorption line at 7187.38 A, which is a blend of a solar iron line and a terrestrial water-vapor line, the shift is sufficient for the iron line to form a new blend with the H2) line at 7187.01 A and thereby alter the relative strengths of the lines (compare adjacent spectrum of the moon). If oxygen or water-vapor lines were present in these Martian spectra, they ought to appear as faint companions to the corresponding lines produced by the earth's atmosphere, but no such companion lines are to be seen.
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Source National Institute of Standards and Technology
Author National Institute of Standards and Technology
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This image is in the public domain in the United States because it is a work of the United States Federal Government, specifically an employee of the National Institute of Standards and Technology, under the terms of Title 17, Chapter 1, Section 105 of the US Code.

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Public domain
This image is in the public domain in the United States because it is a work of the United States Federal Government, specifically an employee of the National Institute of Standards and Technology, under the terms of Title 17, Chapter 1, Section 105 of the US Code.

English  日本語  македонски  Nederlands  +/−

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current15:37, 11 March 2014Thumbnail for version as of 15:37, 11 March 20145,993 × 4,779 (20.72 MB)NISTResearchLibrary (talk | contribs)

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