contributor author | Harris, D. Lee | |
date accessioned | 2017-06-09T14:13:56Z | |
date available | 2017-06-09T14:13:56Z | |
date copyright | 1966/11/01 | |
date issued | 1966 | |
identifier issn | 0022-4928 | |
identifier other | ams-15256.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150908 | |
description abstract | By photographing the movement of smoke plumes and recording the air movement at fixed points above the water in an indoor wave tank, it is shown that progressive waves in water may produce an airflow more than half a wavelength, or 14 wave amplitudes, above the water. The significance of this finding is that it indicates that the mean wind speed should not vanish at the mean water surface as is commonly assumed, and that the vertical gradient of the horizontal wind near the surface of water covered by progressive waves should be less than the gradient near a land surface with other conditions nearly identical. | |
publisher | American Meteorological Society | |
title | The Wave-Driven Wind | |
type | Journal Paper | |
journal volume | 23 | |
journal issue | 6 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1966)023<0688:TWDW>2.0.CO;2 | |
journal fristpage | 688 | |
journal lastpage | 693 | |
tree | Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 006 | |
contenttype | Fulltext | |