| dc.contributor.author | Godson, W. L. | |
| dc.date.accessioned | 2017-06-09T14:11:20Z | |
| dc.date.available | 2017-06-09T14:11:20Z | |
| dc.date.copyright | 1955/12/01 | |
| dc.date.issued | 1955 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-14213.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149750 | |
| dc.description.abstract | The calculation of transmission for a model spectrum requires the adoption of a distribution function for line intensity. In the case of the infrared water-vapor spectrum (random model), a logarithmic ogive distribution for line intensity is very realistic and produces smaller transmission and cooling-rate errors than other functions previously proposed. These results apply also when experimental data are assumed available and the requisite parameters are obtained by curve fitting. | |
| dc.publisher | American Meteorological Society | |
| dc.title | THE COMPUTATION OF INFRARED TRANSMISSION BY ATMOSPHERIC WATER VAPOR, PART II | |
| dc.type | Journal Paper | |
| dc.journal.volume | 12 | |
| dc.journal.issue | 6 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1955)012<0533:TCOITB>2.0.CO;2 | |
| dc.journal.fristpage | 533 | |
| dc.journal.lastpage | 535 | |
| dc.tree | Journal of Meteorology:;1955:;volume( 012 ):;issue: 006 | |
| dc.contenttype | Fulltext | |
