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- W996984472 abstract "The quality of scaling in different observables is discussed. For the characterization and understanding of fully developed turbu lence noticeable attention is paid to scaling behavior. We will discuss and compare some scaling observables. The most frequent used quantities to illustrate scaling in fully de veloped turbulence are the structure functions Sn == ((e; . (v(i + r') v(i)))n) ex: r{n . But even for very high Reynolds number turbulent flows the scaling range for structure functions is very short and additional manipulation of the data like extended self similarity or SO(3) decom position have been applied to extend the scaling range. This leads us to the question if not other observables or other fields are better suited to investigate scaling. We will illustrate the scaling behavior of different observables for two different sets of data, an atmospheric boundary layer recorded under nominally steady condition and a cryogenic helium jet. The atmospheric boundary layer was recorded on top of a meteoro logical tower at about 35m above ground. The Reynolds number for this data set based on the Taylor microscale ). = J(u 2)/{(8u/8x)2)" @default.
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- W996984472 date "2004-01-01" @default.
- W996984472 modified "2023-09-27" @default.
- W996984472 title "News About the Intermittency Exponent" @default.
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- W996984472 doi "https://doi.org/10.1007/978-94-007-0997-3_42" @default.
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