Generation of Surface Waves on a Rotating Sea by Wind Stress: Exploring the dynamics of surface waves in the Chesapeake Bay

Abstract

The work of surface gravitational waves to determine the motion of the air-sea force is being studied in the central region of the Chesapeake Bay. The observed wave spectra showed that the course of the waves in the Chesapeake Bay is closely related to the mathematics of the bowl. Waves directed only at the maximum input suggest that all wave frequencies can be bent steadily and enthusiastically towards a nearby wind. “The direct differentiation of a Ultrasonic anemometer and a vertical AVD cluster show that the size and pattern of the pressure factor across the air-sea interface have changed, suggesting that pressure factor differentiation has occurred on or near the water surface. Using a digital wave model in combination with direct motion assessments, the air-sea force motion was split between the surface acoustic wave field and the mean current. The results show that the surface wave field can store or carry much of the energy development on a dimensional scale, depending on the direction of the breeze. When the wind blew on the victorious wells, about 40 of the total wind pressure was carried away by the short period of the gravitational waves. Considering the power limit in the area of surface waves, the monetary adjustment of air-sea energy has been completed. Understanding between the history of the Lagrange cut and the direction of the pressure factor vector in the mixed surface layer suggests the saw's directional differentiation is a result of the combined effect of the breakwater and fire accounting for slippery energy surfaces. In the direction of the field of the vortex of the expanding wave in a shape similar to the Langmuir roughness”.