The Share of the Mean Turbulent Kinetic Energy in the Near-Neutral Surface Layer for High and Low Wind Speeds
We examine the dependence on wind speed of the share of the mean turbulent kinetic energy among the three velocity components in the near-neutral surface layer. To contrast the general behaviour and the local effects, four datasets are considered, corresponding to different surfaces and environmenta...
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| Published in | Boundary-layer meteorology Vol. 172; no. 1; pp. 81 - 106 |
|---|---|
| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Dordrecht
Springer Netherlands
01.07.2019
Springer Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
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| Abstract | We examine the dependence on wind speed of the share of the mean turbulent kinetic energy among the three velocity components in the near-neutral surface layer. To contrast the general behaviour and the local effects, four datasets are considered, corresponding to different surfaces and environmental conditions. For high wind speeds (i.e., wind speed
≈
10
ms
-
1
), the shares are well-defined and about the same for all sites. As wind speed decreases (becoming
≈
1
ms
-
1
), large record-to-record variability occurs giving, on average, an almost isotropic state for the horizontal velocity components. Through spectral analysis, we relate this behaviour to the low-frequency, submeso motions and to the lack of conditions required by Reynolds averaging. The implications for modelling are also discussed, showing that the wind speed, or a related quantity, must be accounted for, besides stability, in second-order closures. |
|---|---|
| AbstractList | We examine the dependence on wind speed of the share of the mean turbulent kinetic energy among the three velocity components in the near-neutral surface layer. To contrast the general behaviour and the local effects, four datasets are considered, corresponding to different surfaces and environmental conditions. For high wind speeds (i.e., wind speed \[\approx {10}\,{\hbox {ms}^{-1}}\]), the shares are well-defined and about the same for all sites. As wind speed decreases (becoming \[\approx {1}\,{\hbox { ms}^{-1}}\]), large record-to-record variability occurs giving, on average, an almost isotropic state for the horizontal velocity components. Through spectral analysis, we relate this behaviour to the low-frequency, submeso motions and to the lack of conditions required by Reynolds averaging. The implications for modelling are also discussed, showing that the wind speed, or a related quantity, must be accounted for, besides stability, in second-order closures. We examine the dependence on wind speed of the share of the mean turbulent kinetic energy among the three velocity components in the near-neutral surface layer. To contrast the general behaviour and the local effects, four datasets are considered, corresponding to different surfaces and environmental conditions. For high wind speeds (i.e., wind speed ≈ 10 ms - 1 ), the shares are well-defined and about the same for all sites. As wind speed decreases (becoming ≈ 1 ms - 1 ), large record-to-record variability occurs giving, on average, an almost isotropic state for the horizontal velocity components. Through spectral analysis, we relate this behaviour to the low-frequency, submeso motions and to the lack of conditions required by Reynolds averaging. The implications for modelling are also discussed, showing that the wind speed, or a related quantity, must be accounted for, besides stability, in second-order closures. We examine the dependence on wind speed of the share of the mean turbulent kinetic energy among the three velocity components in the near-neutral surface layer. To contrast the general behaviour and the local effects, four datasets are considered, corresponding to different surfaces and environmental conditions. For high wind speeds (i.e., wind speed [Formula omitted]), the shares are well-defined and about the same for all sites. As wind speed decreases (becoming [Formula omitted]), large record-to-record variability occurs giving, on average, an almost isotropic state for the horizontal velocity components. Through spectral analysis, we relate this behaviour to the low-frequency, submeso motions and to the lack of conditions required by Reynolds averaging. The implications for modelling are also discussed, showing that the wind speed, or a related quantity, must be accounted for, besides stability, in second-order closures. |
| Audience | Academic |
| Author | Yagüe, C. Mazzola, M. Tampieri, F. Bosveld, F. C. Schiavon, M. Viola, A. P. Castelli, S. Trini |
| Author_xml | – sequence: 1 givenname: M. orcidid: 0000-0002-3564-7512 surname: Schiavon fullname: Schiavon, M. email: mario.schiavon2@unibo.it organization: Department of Physics and Astronomy, Univeristy of Bologna, Institute of Atmospheric Sciences and Climate - ISAC-CNR – sequence: 2 givenname: F. surname: Tampieri fullname: Tampieri, F. organization: Institute of Atmospheric Sciences and Climate - ISAC-CNR – sequence: 3 givenname: F. C. surname: Bosveld fullname: Bosveld, F. C. organization: Royal Netherlands Meteorological Institute – sequence: 4 givenname: M. surname: Mazzola fullname: Mazzola, M. organization: Institute of Atmospheric Sciences and Climate - ISAC-CNR – sequence: 5 givenname: S. Trini surname: Castelli fullname: Castelli, S. Trini organization: Institute of Atmospheric Sciences and Climate - ISAC-CNR – sequence: 6 givenname: A. P. surname: Viola fullname: Viola, A. P. organization: Institute of Atmospheric Sciences and Climate - ISAC-CNR – sequence: 7 givenname: C. surname: Yagüe fullname: Yagüe, C. organization: Dpt. Física de la Tierra y Astrofísica, Facultad de CC. Físicas, Universidad Complutense de Madrid |
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| CitedBy_id | crossref_primary_10_1007_s10652_021_09800_x crossref_primary_10_1007_s42865_023_00055_6 crossref_primary_10_3390_atmos12091095 crossref_primary_10_1007_s10546_021_00678_2 crossref_primary_10_1007_s10546_022_00774_x crossref_primary_10_5194_acp_23_7425_2023 |
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| Keywords | Low wind speed Turbulent kinetic energy Submeso motions Velocity spectra Dissipation rate |
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| SubjectTerms | Analysis Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Closures Components Dependence Earth and Environmental Science Earth Sciences Environmental conditions Force and energy Kinetic energy Low wind speeds Meteorology Modelling Research Article Reynolds averaging Spectral analysis Stability Surface boundary layer Surface layers Turbulent kinetic energy Velocity Wind Wind speed |
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| Title | The Share of the Mean Turbulent Kinetic Energy in the Near-Neutral Surface Layer for High and Low Wind Speeds |
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