| dc.contributor.author | Fleagle, Robert G. | |
| dc.date.accessioned | 2017-06-09T14:11:24Z | |
| dc.date.available | 2017-06-09T14:11:24Z | |
| dc.date.copyright | 1956/04/01 | |
| dc.date.issued | 1956 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-14243.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149783 | |
| dc.description.abstract | Theoretical considerations suggest that the temperature distribution within a meter of a cold surface may be partially stratified as a result of radiative and turbulent processes. Even though stratification would be of crucial importance in certain boundary-layer processes, it probably would be undetectable by conventional thermometry. Observations using direct refractive thermometry have been used to determine with great accuracy the temperature distribution above a cold water surface. These observations reveal a persistent temperature anomaly about 10 centimeters above the surface, which is consistent with theory. | |
| dc.publisher | American Meteorological Society | |
| dc.title | THE TEMPERATURE DISTRIBUTION NEAR A COLD SURFACE | |
| dc.type | Journal Paper | |
| dc.journal.volume | 13 | |
| dc.journal.issue | 2 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1956)013<0160:TTDNAC>2.0.CO;2 | |
| dc.journal.fristpage | 160 | |
| dc.journal.lastpage | 165 | |
| dc.tree | Journal of Meteorology:;1956:;volume( 013 ):;issue: 002 | |
| dc.contenttype | Fulltext | |
