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First the mean horizontal speeds of the inner and outer radii are taken from the inclination of the above mentioned linear regression lines: v inner =d R inner /d t=240 m/s, v outer =d R outer /d t= 170 m/s.
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The slope of the regression line implies a mean horizontal speed of 2.3 km/s along the surface, which is within the range of Rayleigh wave speeds.
It means that the initial average horizontal speed is 52.7 m.
The mean horizontal velocity is 210 ms−1.
Indeed, the maximum horizontal speed attained in their 0.4 m cube (1.2 ms−1) was the same as the mean horizontal flight speed in our 1.6 m cube (1.2 ms−1.2
The study site is a tidal strait that exhibits semi-diurnal tidal current characteristics, with a mean horizontal current speed of 1.4 m s−1, and a turbulence intensity of 15% at a reference mean current of 2 m s−1.
The results show that both the tracked epicenter and the tsunami origin are quite close to the epicenter reported by the USGS, with a mean horizontal propagation speed of 2.3 km/s after the earthquake and about 210 m/s after the tsunami.
The mean horizontal flight speed was 1.2 ms.d (s.d. = 0.5 ms−1), with a maximum of 2.4 ms−1.
Then the mean of the above calculated horizontal speeds is taken 〈v〉=(v inner +v outer )/2≈200 m/s.
Third, texture, by which I mean horizontal richness: layer on layer of history.
Production of wave-induced mean jets and their superposition with nonlinear unstable dissipative AGWs can produce strong narrow peaks of horizontal speed in the upper atmosphere.
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