Coriolis effect, the apparent deflection of moving objects from a straight path when viewed from a rotating frame of reference
Henry Stommel showed that the north-south gradient of the strength of the Coriolis force (the "beta effect") was responsible for the observed fact that the return flow of the slow interior gyre circulations is concentrated in fast moving western boundary currents, such as the Gulf Stream and the Kuroshio Current, a process known as western intensification.
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More about the combined effects of wind loads and upthrust is discussed later, under the section of "Heave and roll behavior" which would describe the similar of a spar-buoy on a waterway and on the section "Wind force and Coriolis", likewise for bending and deflection on the structure.