High-temperature, high-resolution photoabsorption cross sections of O2in the 108.5-nm region
Autor: | Tom Hung, Takashi Matsui, C. Y. Robert Wu, D. L. Judge |
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Rok vydání: | 2001 |
Předmět: |
Atmospheric Science
Materials science Absorption spectroscopy Soil Science High resolution Aquatic Science Oceanography Optics Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Absorption (electromagnetic radiation) Earth-Surface Processes Water Science and Technology Ecology business.industry Resolution (electron density) Airglow Paleontology Forestry Geophysics Space and Planetary Science Satellite Ionosphere Thermosphere Atomic physics business |
Zdroj: | Journal of Geophysical Research: Space Physics. 106:5599-5603 |
ISSN: | 0148-0227 |
DOI: | 10.1029/2000ja000360 |
Popis: | The high-resolution absorption cross-section measurements of O2 in the 108.0- to 108.7-nm spectral region have been carried out with a resolution of 0.0008 nm and at temperatures of 295 and 535 K. The absorption features in this spectral region exhibit primarily a blue-shaded broad band with a band head peaked at 108.52 nm. The center of gravity of the diffuse band is located at 108.452 nm. The present room temperature cross-section data of the NII 108.5-nm sextuplets agree well with the unpublished data of J.A.R. Samson (private communication, 1990). As the temperature increases from 295 to 535 K, we observe a decrease in cross-section values by as much as 30% over the contour of the diffuse band. Similarly, the cross-section values of the sharp features decrease as temperature increases. The NII 108.5-nm multiplets are one of the prominent emissions in the Earth's airglow. The EUV-UV day glow limb scans of the thermosphere and ionosphere have currently been gathered by satellite, e.g., ARGOS, at a tangent ray height of 200 km, above where the ambient absorption due to O2 and N2 is expected. The present temperature-dependent cross sections of O2 provide the important database required for modeling the dayglow observations. |
Databáze: | OpenAIRE |
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