Regions ofintensive wave growth are observed in the northwest Pacific, the northwest Atlantic, the Southern Ocean, and the Mediterranean Sea. Seasonality is distinct for the climate of both swell and wind sea, notably the large-scale northward bending of the swell pools in boreal summer, and ...
A detailed climatology of wind sea and swell waves in the Nordic Seas (North Sea, Norwegian Sea, and Barents Sea), based on the high-resolution reanalysis NORA10, developed by the Norwegian Meteorological Institute, is presented. The higher resolution of the wind forcing fields, and the wave ...
The Air–Sea Momentum Flux in Conditions of Wind Sea and Swell During the Surface Wave Dynamics Experiment, direct measurements of momentum, heat, and water vapor fluxes were obtained from a mast on the foredeck of a S... MA Donelan,WM Drennan,KB Katsaros - 《Journal of Physical ...
A severe depth-limited storm and a case of extreme swell, both of which occurred in the North Sea, were hindcasted with a regional version of the third-generation WAM wave model. Two different expressions for the bottom dissipation source term were used; the Hasselman and Collins drag-law ...
In this paper, different partitioning techniques and methods to identify wind sea and swell are investigated, addressing both 1D and 2D schemes. Current partitioning techniques depend largely on arbitrary parameterizations to assess if wave systems are significant or spurious. This makes the implementation...
Regions ofintensive wave growth are observed in the northwest Pacific, the northwest Atlantic, the Southern Ocean, and the Mediterranean Sea. Seasonality is distinct for the climate of both swell and wind sea, notably the large-scale northward bending of the swell pools in boreal summer, and ...
1) wind-sea/swell regime 海面状况1. The fraction velocities in different wind-sea/swell regimes are calculated by using six different turbulent flux parameterization schemes,where the dada collected from the surface wave dynamics experiment are used. 结果表明:海面状况对计算结果有显著影响,六种参数...
doi:10.1029/EO051i007p00544T. P. BarnettJohn Wiley & Sons, Ltd.Eos Transactions American Geophysical UnionBarnett, T. P., 1970: Wind waves and swell in the North Sea. Eos, Wash. 51 , 544.
Modeling analysis of the swell and wind-sea climate in the Salish Sea. Estuarine Coast. Shelf Sci. 224, 289–300 (2019). Google Scholar Coppola, E. et al. A first-of-its-kind multi-model convection permitting ensemble for investigating convective phenomena over Europe and the Mediterranean....
In comparison to the other data sources these data have the longest records and provide independent estimates of wind sea and swell. Gulev and Grigorieva (2004) using longer time collection developed 120-year long time series of SWH for well sampled areas of the location of major ship routes....