Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Paul Wittmann"'
Publikováno v:
Journal of Geophysical Research: Oceans. 118:6329-6348
[1] Multiyear climate variations influence North Pacific storm intensity and resultant variations in wave energy levels. The timing of these decadal fluctuations and strong El Nino's have had a strong influence on long-term trends. Here we investigat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72ce3d2178a1fef8d9dedc025330656d
https://doi.org/10.1002/2013jc009189
https://doi.org/10.1002/2013jc009189
Autor:
Natacha B. Bernier, Jose-Henrique G. M. Alves, Jessica Schauer, Paul Wittmann, Jamie McLean, Scott Stripling, Yung Chao, Stephen Klotz, Arun Chawla, Michael Sestak, Glenn Nelson, Hendrik L. Tolman
Publikováno v:
Bulletin of the American Meteorological Society. 94:1893-1905
The U.S. National Centers for Environmental Prediction (NCEP) and the Fleet Numerical Meteorology and Oceanography Center (FNMOC) have joined forces to establish a first global multicenter ensemble system dedicated to probabilistic forecasts of windw
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e9454011c938a3658941d4b6057a09e
https://doi.org/10.1175/bams-d-12-00032.1
https://doi.org/10.1175/bams-d-12-00032.1
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 11:506-524
During the period 20-23 September 1990, the remnants of Supertyphoon Flo moved into the central North Pacific Ocean with sustained wind speeds of 28 m/s. The strong wind and large fetch area associated with this storm generated long-period swell that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c07871b923b70f4eced49d92d9286fa
https://doi.org/10.1175/1520-0426(1994)011<0506:aapoos>2.0.co
https://doi.org/10.1175/1520-0426(1994)011<0506:aapoos>2.0.co
Publikováno v:
Geophysical Research Letters. 36
[1] The turbulent Reynolds stresses in the upper layers of the ocean interact with the vertical shear of the Stokes drift velocity of the wave field to extract energy from the surface waves. The resulting rate of dissipation of wind waves in the glob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07a49ada38cdbfcfc5f1c270468d169f
https://doi.org/10.1029/2008gl036193
https://doi.org/10.1029/2008gl036193
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