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.

Bibliographic Details
Published in:Science
Main Author: Murcray, W. B.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1963
Subjects:
Arctic
Arctic Ocean
Online Access:http://dx.doi.org/10.1126/science.141.3583.802
https://www.science.org/doi/pdf/10.1126/science.141.3583.802
id craaas:10.1126/science.141.3583.802
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spelling craaas:10.1126/science.141.3583.802 2024-06-09T07:43:08+00:00 Infrared Radiation from the Atmosphere over the Arctic Ocean Murcray, W. B. 1963 http://dx.doi.org/10.1126/science.141.3583.802 https://www.science.org/doi/pdf/10.1126/science.141.3583.802 en eng American Association for the Advancement of Science (AAAS) Science volume 141, issue 3583, page 802-804 ISSN 0036-8075 1095-9203 journal-article 1963 craaas https://doi.org/10.1126/science.141.3583.802 2024-05-16T12:56:03Z 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. Article in Journal/Newspaper Arctic Arctic Ocean AAAS Resource Center (American Association for the Advancement of Science) Arctic Arctic Ocean Science 141 3583 802 804
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description 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.
format Article in Journal/Newspaper
author Murcray, W. B.
spellingShingle Murcray, W. B.
Infrared Radiation from the Atmosphere over the Arctic Ocean
author_facet Murcray, W. B.
author_sort Murcray, W. B.
title Infrared Radiation from the Atmosphere over the Arctic Ocean
title_short Infrared Radiation from the Atmosphere over the Arctic Ocean
title_full Infrared Radiation from the Atmosphere over the Arctic Ocean
title_fullStr Infrared Radiation from the Atmosphere over the Arctic Ocean
title_full_unstemmed Infrared Radiation from the Atmosphere over the Arctic Ocean
title_sort infrared radiation from the atmosphere over the arctic ocean
publisher American Association for the Advancement of Science (AAAS)
publishDate 1963
url http://dx.doi.org/10.1126/science.141.3583.802
https://www.science.org/doi/pdf/10.1126/science.141.3583.802
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source Science
volume 141, issue 3583, page 802-804
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.141.3583.802
container_title Science
container_volume 141
container_issue 3583
container_start_page 802
op_container_end_page 804
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