The pattern of radiative heating and cooling in the troposphere and lower stratosphere
For any meteorological effects of radiation, only those constituents of the air which have a very strong absorption in the infra-red are involved; these are water vapour and carbon dioxide. Several methods have been developed (Mügge & Möller 1932 a, b Elsasser 1942; Yamamoto 1952) for computing...
| Published in: | Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
The Royal Society
1956
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1098/rspa.1956.0121 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.1956.0121 |