wind stress वाक्य
उदाहरण वाक्य
मोबाइल
- Aside from the oscillatory motions associated with curl of the wind stress.
- Equatorial Kelvin waves are often associated with anomalies in surface wind stress.
- The cantilevers were to be splayed, to take account of horizontal wind stresses.
- Wind stress acting on the surface generates currents, which have not been well described.
- Architects and accountants now have spreadsheets for everything from wind stress to foreign tax shelters.
- Turbulent eddies can also be produced from wind stress by the atmosphere on the ocean.
- Also, wind stresses the rigging of sailing ships.
- Giles et al . ( 2012 ) conclude that the variability in freshwater content varies with wind stress curl.
- Through the wind stress, the wind generates ocean surface waves; the longer waves have a phase velocity tending towards the wind speed.
- Oceanic currents are largely driven by the surface wind stress; hence the large-scale atmospheric circulation is important to understanding the ocean circulation.
- The NECC is a direct response to the meridional change of the wind stress curl near the Intertropical Convergence Zone ( ITCZ ).
- However, upon entering a shallow, gently sloping shelf, the surge cannot be dispersed, but is driven ashore by the wind stresses of the hurricane.
- The wind stress also generates turbulence, which causes the surface fresh water to be mixed down and results in a brackish layer typically thick.
- The NECC is an interesting case because while it results from wind-driven circulation, it transports water against the mean westward wind stress in the tropics.
- The areas of most positive wind stress curl are characterized by very weak sea surface temperature incline, and are likely consistent to regions of mode water.
- A . Storm surge : A rise of water above normal level along a shore due to the action of wind stress on the water surface.
- The AMOC is calculated on the basis of the directly measured boundary currents, the geostrophic currents and the Ekman transports estimated from the surface wind stress.
- Some work had already been carried out by Eug�ne Viollet-Le-Duc, but he had died in 1879 . Eiffel was selected because of his experience with wind stresses.
- The wind-driven horizontal transport in the mixed layer is approximately described by Ekman Layer dynamics in which vertical diffusion of momentum balances the Coriolis effect and wind stress.
- This apparent paradox is concisely explained by Sverdrup theory, which shows that the east-west transport is governed by the north-south change in the curl of the wind stress.
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