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Further support to Kolmogoroff's theory of local isotropy is provided by hot-wire measurements of fluctuations of downwind velocities at a height of 1 to 2 m above the sea surface. The results agree with those obtained from observations made in a tidal stream by Grant, Stewart and Moilliet (1962) and with measurements of skewness of velocity differences in air over land, made by Gurvich (1960).
Further support to Kolmogoroff's theory of local isotropy is provided by hot-wire measurements of fluctuations of downwind velocities at a height of 1 to 2 m above the sea surface. The results agree with those obtained from observations made in a tidal stream by Grant, Stewart and Moilliet (1962) and with measurements of skewness of velocity differences in air over land, made by Gurvich (1960).
| All Time | Past Year | Past 30 Days | |
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| Full Text Views | 347 | 47 | 8 |
| PDF Downloads | 126 | 37 | 4 |
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