Observations of the Response of Sea Waves to Veering WindsSource: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 012::page 1876Author:Masson, Diane
DOI: 10.1175/1520-0485(1990)020<1876:OOTROS>2.0.CO;2Publisher: American Meteorological Society
Abstract: A data-adaptive technique, the iterative maximum likelihood method, is used to estimate directional wave spectra from data collected by three pitch-and-roll buoys, during two turning wind events of the CASP 86 experiment. A relaxation coefficient is estimated for the response of both the mean wave direction for each frequency band and the main wave direction of the wind sea spectrum to a change in wind direction. The values of the coefficients are found to be consistent with each other, and within the scatter of previous estimates. Also, a definite correlation is established between the wave rms angular spread and the rate of change of wind direction. Finally, the shapes of the estimated directional distributions are tested for symmetry and unimodality. A significant proportion of the estimated distributions are found to be neither unimodal nor symmetric.
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contributor author | Masson, Diane | |
date accessioned | 2017-06-09T14:49:49Z | |
date available | 2017-06-09T14:49:49Z | |
date copyright | 1990/12/01 | |
date issued | 1990 | |
identifier issn | 0022-3670 | |
identifier other | ams-27712.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4164748 | |
description abstract | A data-adaptive technique, the iterative maximum likelihood method, is used to estimate directional wave spectra from data collected by three pitch-and-roll buoys, during two turning wind events of the CASP 86 experiment. A relaxation coefficient is estimated for the response of both the mean wave direction for each frequency band and the main wave direction of the wind sea spectrum to a change in wind direction. The values of the coefficients are found to be consistent with each other, and within the scatter of previous estimates. Also, a definite correlation is established between the wave rms angular spread and the rate of change of wind direction. Finally, the shapes of the estimated directional distributions are tested for symmetry and unimodality. A significant proportion of the estimated distributions are found to be neither unimodal nor symmetric. | |
publisher | American Meteorological Society | |
title | Observations of the Response of Sea Waves to Veering Winds | |
type | Journal Paper | |
journal volume | 20 | |
journal issue | 12 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1990)020<1876:OOTROS>2.0.CO;2 | |
journal fristpage | 1876 | |
journal lastpage | 1885 | |
tree | Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 012 | |
contenttype | Fulltext |