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Date : 2001-09-24
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Wind stress Wikipedia ~ In physical oceanography and fluid dynamics the wind stress is the shear stress exerted by the wind on the surface of large bodies of water – such as oceans seas estuaries and lakes It is the force component parallel to the surface per unit area as applied by the wind on the water surface
Wind Stress over the Ocean Ian S F Jones 9780521090490 ~ Parameterization of the wind stress over the ocean is central to many facets of airsea interaction which in turn is vital for models of weather prediction and climate modeling Wind Stress over the Ocean brings together thirty of the worlds leading experts in airsea interaction to provide a thorough reexamination of the physical processes that transfer momentum between the atmosphere and the ocean
Wind Stress an overview ScienceDirect Topics ~ Furthermore wind energy input into surface waves is a strong nonlinear function of wind stress so that the high frequency components of wind stress make a critical part of contribution to the wind energy input into the ocean Although monthly mean wind stress can be used to calculate the winddriven circulation with reasonable results mixed layer property calculation requires wind stress products with high temporal resolution up to 6hourly wind
Wind Stress Over the Ocean Oceanography ~ The monograph is the final report of the Scientific Committee on Oceanographic Research SCOR working group 101 which was commissioned in 1993 to survey the state of knowledge and suggest where research might be directed on the topic of stress over the ocean
Oct 14 The upper ocean response to winds ~ Wind stress and drag coefficients Wind blowing over the sea surface exerts a stress on the ocean that imparts momentum This drag force at the surface slows the wind speed and forms a boundary layer in the atmosphere
Wind Stress Drag Coefficient over the Global Ocean ~ In particular the total wind stress magnitude τ at the ocean surface can be calculated from the square of the wind speed at 10 m above the sea surface V a the density of air ρ a and a dimensionless drag coefficient C D with τ ρ a C D V 2 a
Coupled effects of ocean current on wind stress in the Bay ~ According to the bulk aerodynamic formula the wind stress τ is calculated as1τρaCDua−uoua−uowhere ρ a the density of the air C D the drag coefficient u a and u o the wind and ocean surface current velocity respectively
Wind Stress and Heat Flux over the Ocean in Gale Force ~ Data from this platform have been analyzed by the eddy correlation method to obtain wind stress and heat flux at wind speeds from 6 to 22 m s −1 in a deepwater wave regime significantly extending the range of available measurements The sea surface drag coefficient increases gradually with increasing wind speed
Introduction to Physical Oceanography ~ Wind blowing over the sea surface exerts a stress on the ocean that imparts momentum This drag force at the surface slows the wind speed and forms a boundary layer in the atmosphere The precise details of how the atmosphere and ocean interact to exchange momentum is complicated by the stratification or stability of the atmospheric boundary layer the presence of waves wave breaking and a host of other processes
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