Infrared Radiation from the Atmosphere over the Arctic Ocean
The emission spectrum of the atmosphere over the Arctic Ocean was observed during a period when atmosphere and snow surface temperatures were about -40°C. The main contributions to the emission in the 5- to 21-micron range came from ozone and carbon dioxide, with water vapor playing a minor part.
| Published in: | Science |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
American Association for the Advancement of Science (AAAS)
1963
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1126/science.141.3583.802 https://www.science.org/doi/pdf/10.1126/science.141.3583.802 |
| Summary: | The emission spectrum of the atmosphere over the Arctic Ocean was observed during a period when atmosphere and snow surface temperatures were about -40°C. The main contributions to the emission in the 5- to 21-micron range came from ozone and carbon dioxide, with water vapor playing a minor part. |
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