Zobrazeno 1 - 10
of 113
pro vyhledávání: '"Mark A. Donelan"'
Autor:
Mark A. Donelan, William J. Plant
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 37:67-83
We describe here a method for recovering directional ocean surface wave spectra obtained from height and slope measurements made over a small area, the iterative deconvolution method (IDM). We show that IDM is a more reliable method for estimating di
Autor:
Mark A. Donelan, Ian R. Young
Publikováno v:
Remote Sensing of Environment. 215:228-241
Three extensive global wind speed and wave height datasets (altimeter, radiometer, model reanalysis) are analysed to investigate the global wind speed and wave height climate. Despite the fact that these datasets have all been carefully calibrated, t
Autor:
Mark A. Donelan
Publikováno v:
Journal of Geophysical Research: Oceans. 123:1485-1501
Publikováno v:
Journal of Geophysical Research: Oceans. 122:10174-10183
Tropical storm intensity prediction remains a challenge in tropical meteorology. Some tropical storms undergo dramatic rapid intensification and rapid decline. Hurricane researchers have considered particular ambient environmental conditions includin
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 34:1225-1234
There exists considerable disagreement among the observed values of the drag coefficient CD. To develop a model of CD, the wind stress generally will be calculated from the eddy correlation method. A buoy is suitable to measure the wind stress in man
Publikováno v:
Journal of Physical Oceanography. 46:2143-2156
Measurements of pressure near the surface in conditions of wind sea and swell are reported. Swell, or waves that overrun the wind, produces an upward flux of energy and momentum from waves to the wind and corresponding attenuation of the swell waves.
Publikováno v:
Journal of Geophysical Research: Oceans. 120:5040-5053
Three methods of estimating the directional spectra of water waves are intercompared. The Maximum Likelihood Method (MLM) and the Maximum Entropy Method (MEM) require stationarity of the time series and yield only the frequency-direction spectra. The
Publikováno v:
Icarus (N.Y.N.Y. 1962) 250 (2015): 368–383. doi:10.1016/j.icarus.2014.12.001
info:cnr-pdr/source/autori:Banfield D.; Donelan M.; Cavaleri L./titolo:Winds, waves and shorelines from ancient martian seas/doi:10.1016%2Fj.icarus.2014.12.001/rivista:Icarus (N.Y.N.Y. 1962)/anno:2015/pagina_da:368/pagina_a:383/intervallo_pagine:368–383/volume:250
info:cnr-pdr/source/autori:Banfield D.; Donelan M.; Cavaleri L./titolo:Winds, waves and shorelines from ancient martian seas/doi:10.1016%2Fj.icarus.2014.12.001/rivista:Icarus (N.Y.N.Y. 1962)/anno:2015/pagina_da:368/pagina_a:383/intervallo_pagine:368–383/volume:250
We consider under what environmental conditions water waves (and thus eventually shorelines) should be expected to be produced on hypothetical ancient martian seas and lakes. For winds and atmospheric pressures that are too small, no waves should be
Publikováno v:
Journal of Oceanography. 71:199-204
We propose a new model with microbreaking and linear dependence on wind speed in the whitecap-free area and linear dependence on the fractional area of whitecaps, based on the whitecap model proposed by Monahan and Spillane (The role of oceanic white
Autor:
Mark A. Donelan
Publikováno v:
Encyclopedia of Maritime and Offshore Engineering
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee2eec0be2a99cbdccf0a1a0ab2fc39d
https://doi.org/10.1002/9781118476406.emoe079
https://doi.org/10.1002/9781118476406.emoe079