| contributor author | Elliott, J. A. | |
| contributor author | Oakey, N. S. | |
| date accessioned | 2017-06-09T14:44:07Z | |
| date available | 2017-06-09T14:44:07Z | |
| date copyright | 1975/07/01 | |
| date issued | 1975 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25531.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162325 | |
| description abstract | Temperature gradient records from vertical lowerings of an array of four thermometers are used to trace microstructure features horizontally over a distance of 46 cm. Identifiable features are found to have a slope and a vertical velocity or curvature with a statistical distribution similar to that expected from an internal wave field superimposed on horizontally-layered microstructure. The horizontal extent of microstructure with a vertical scale greater than 5 cm is at least an order of magnitude greater than its vertical scale. | |
| publisher | American Meteorological Society | |
| title | Horizontal Coherence of Temperature Microstructure | |
| type | Journal Paper | |
| journal volume | 5 | |
| journal issue | 3 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1975)005<0506:HCOTM>2.0.CO;2 | |
| journal fristpage | 506 | |
| journal lastpage | 515 | |
| tree | Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 003 | |
| contenttype | Fulltext | |
