A possible manifestation of double diffusive convection in the atmosphere |
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| Authors: | Francis J Merceret |
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| Institution: | (1) National Hurricane and Experimental Meteorology Laboratory, Coral Gables, Florida, USA |
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| Abstract: | Small-scale turbulence measurements above the top of the boundary layer in Hurricane Eloise (1975) showed an anomalous peak in the power spectrum of horizontal velocity fluctuation at a scale of 20 cm. Double diffusive convection is suggested as the most reasonable explanation for the presence of the peak. |
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