Mars: The Origin of the 3.58- and 3.69-Micron Minima in the Infrared Spectra
- 12 March 1965
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 147 (3663), 1286-1288
- https://doi.org/10.1126/science.147.3663.1286
Abstract
The 3- to 4-micron spectra of Mars, recorded with the 200-inch telescope in 1958, were reexamined in order to ascertain whether the minima at 3.58 and 3.69 microns are due to telluric HDO molecules. Solar spectra obtained at Denver and water vapor abundances derived from radiosonde flights during the observing period were used. There seems to be a correlation between the intensities of the 3.58- and 3.69-micron features and the amount of telluric water vapor in the optical path. An important corollary is that there is no evidence for attributing these spectral features to Mars.Keywords
This publication has 9 references indexed in Scilit:
- Sinton Bands: Evidence for Deuterated Water on MarsScience, 1965
- Interpretation of the 3-to 4-Micron Infrared Spectrum of MarsScience, 1963
- Infrared Transmission of the Atmosphere to Solar RadiationApplied Optics, 1963
- Response : Communication ChannelsScience, 1961
- Solar and stellar abundances of the elementsPhysics and Chemistry of the Earth, 1961
- Further Evidence of Vegetation on MarsScience, 1959
- Spectroscopic Evidence for Vegetation on Mars.The Astrophysical Journal, 1957
- INFRARED DETERMINATION OF PRECIPITABLE WATER VAPOR IN A VERTICAL COLUMN OF THE EARTH'S ATMOSPHEREJournal of Meteorology, 1956
- A Grating Map of the Solar Spectrum from 3.0 to 5.2 Microns.The Astrophysical Journal, 1951