Preprints
https://doi.org/10.5194/egusphere-2024-1366
https://doi.org/10.5194/egusphere-2024-1366
05 Jun 2024
 | 05 Jun 2024

The ratio of transverse to longitudinal turbulent velocity statistics for aircraft measurements

Jakub L. Nowak, Marie Lothon, Donald H. Lenschow, and Szymon P. Malinowski

Abstract. The classical theory of homogeneous isotropic turbulence predicts the ratio of transverse to longitudinal structure functions or power spectra equal to 4/3 in the inertial subrange. For the typical turbulence cascade in the inertial subrange, it also predicts a power law scaling with an exponent of +2/3 and −5/3 for the structure functions and the power spectra, respectively.

We estimate those ratios and exponents from in-situ high-rate turbulence measurements collected by three research aircraft during four field experiments in two regimes of the marine atmospheric boundary layer: shallow trade-wind convection and subtropical stratocumulus. The results were derived by fitting power law formulas to the structure functions and power spectra computed separately for the three components of the turbulent wind velocity measured in horizontal flight segments.

The variability in the results can be attributed to how the wind velocity components are measured on an individual aircraft. The differences related to environmental conditions, e.g. between characteristic levels and regimes of the boundary layer, are of secondary importance.
Experiment-averaged transverse-to-longitudinal ratios are 23–46 % smaller than predicted by the theory. The deviations of average scaling exponents with respect to the theoretical values range from −35 to +47 % for structure functions and from −25 to +22 % for power spectra, depending on experiment and velocity component. The reason for the disagreement in transverse-to-longitudinal ratios between the observations and the theory remains uncertain.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Jakub L. Nowak, Marie Lothon, Donald H. Lenschow, and Szymon P. Malinowski

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1366', Anonymous Referee #1, 26 Jun 2024
    • AC1: 'Reply on RC1', Jakub Nowak, 10 Oct 2024
  • RC2: 'Comment on egusphere-2024-1366', Anonymous Referee #2, 04 Jul 2024
    • AC2: 'Reply on RC2', Jakub Nowak, 10 Oct 2024

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1366', Anonymous Referee #1, 26 Jun 2024
    • AC1: 'Reply on RC1', Jakub Nowak, 10 Oct 2024
  • RC2: 'Comment on egusphere-2024-1366', Anonymous Referee #2, 04 Jul 2024
    • AC2: 'Reply on RC2', Jakub Nowak, 10 Oct 2024
Jakub L. Nowak, Marie Lothon, Donald H. Lenschow, and Szymon P. Malinowski

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The ratio of transverse to longitudinal turbulent velocity statistics for aircraft measurements: software Jakub L. Nowak, Marie Lothon, Donald H. Lenschow, and Szymon P. Malinowski https://doi.org/10.5281/zenodo.11127723

Jakub L. Nowak, Marie Lothon, Donald H. Lenschow, and Szymon P. Malinowski

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Short summary
According to a classical theory, the ratio of turbulence statistics corresponding to transverse and longitudinal wind velocity components equals 4/3 in the inertial range of scales. We analyze large amount of measurements obtained with three research aircraft during four field experiments in different locations and show the observed ratios are almost always significantly smaller. We discuss potential reasons of this disagreement but actual explanation remains to be determined.