### Abstract

Using velocity data obtained in the atmospheric surface layer, we examine Kolmogorovs refined hypotheses. In particular, we focus on the properties of the stochastic variable V=u(r)/(rr)1/3, where u(r) is the velocity increment over a distance r, and r is the dissipation rate averaged over linear intervals of size r. We show that V has an approximately universal probability density function for r in the inertial range and discuss its properties; we also examine the properties of V for r outside the inertial range.

Original language | English (US) |
---|---|

Pages (from-to) | 1178-1181 |

Number of pages | 4 |

Journal | Physical Review Letters |

Volume | 69 |

Issue number | 8 |

DOIs | |

State | Published - 1992 |

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### ASJC Scopus subject areas

- Physics and Astronomy(all)

### Cite this

*Physical Review Letters*,

*69*(8), 1178-1181. https://doi.org/10.1103/PhysRevLett.69.1178

**Kolmogorovs refined similarity hypotheses.** / Stolovitzky, G.; Kailasnath, P.; Sreenivasan, K. R.

Research output: Contribution to journal › Article

*Physical Review Letters*, vol. 69, no. 8, pp. 1178-1181. https://doi.org/10.1103/PhysRevLett.69.1178

}

TY - JOUR

T1 - Kolmogorovs refined similarity hypotheses

AU - Stolovitzky, G.

AU - Kailasnath, P.

AU - Sreenivasan, K. R.

PY - 1992

Y1 - 1992

N2 - Using velocity data obtained in the atmospheric surface layer, we examine Kolmogorovs refined hypotheses. In particular, we focus on the properties of the stochastic variable V=u(r)/(rr)1/3, where u(r) is the velocity increment over a distance r, and r is the dissipation rate averaged over linear intervals of size r. We show that V has an approximately universal probability density function for r in the inertial range and discuss its properties; we also examine the properties of V for r outside the inertial range.

AB - Using velocity data obtained in the atmospheric surface layer, we examine Kolmogorovs refined hypotheses. In particular, we focus on the properties of the stochastic variable V=u(r)/(rr)1/3, where u(r) is the velocity increment over a distance r, and r is the dissipation rate averaged over linear intervals of size r. We show that V has an approximately universal probability density function for r in the inertial range and discuss its properties; we also examine the properties of V for r outside the inertial range.

UR - http://www.scopus.com/inward/record.url?scp=0001341749&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0001341749&partnerID=8YFLogxK

U2 - 10.1103/PhysRevLett.69.1178

DO - 10.1103/PhysRevLett.69.1178

M3 - Article

VL - 69

SP - 1178

EP - 1181

JO - Physical Review Letters

JF - Physical Review Letters

SN - 0031-9007

IS - 8

ER -