Department of Civil and Environmental Engineering Washington State University Pullman WA USA; Institute of Meteorology and Climate Research—Atmospheric Environmental Research Karlsruhe Institute of Technology Karlsruhe Germany; OSTI
Department of Civil and Environmental Engineering Washington State University Pullman WA USA
Department of Civil and Environmental Engineering Duke University Durham NC USA
Department of Earth and Environment Boston University Boston MA USA
In very stable boundary layers (VSBL), a “cocktail” of submeso motions routinely result in elevated mean wind speed maxima above the ground, acting as a new source of turbulence generation. This new source of turbulent kinetic energy enhances turbulent mixing and causes mean wind profile distortion (WPD). As a results, this transient distortion in the wind profile adjusts the classical log‐law. Addressing how WPD‐induced turbulence regulates flow structures, turbulent fluxes, and transitions in stability regimes across layers remains a challenge. Eddy covariance data measured at four levels on a 62‐m tower are employed to address these questions. It is shown that the WPD initiates large turbulent eddies that penetrate downward, leading to enhanced vertical mixing and comparable turbulent transport efficiencies across layers. As a consequence, turbulence intensity and fluxes are increased. As the WPD is intensified, turbulent fluxes and turbulent flux transport caused by large eddies are also enhanced, leading to a transition from very stable to weakly stable regimes. Due to the influence of WPD‐induced large eddies, the large‐eddy turbulent Prandtl number does not deviate appreciably from unity and the partitioning between turbulent kinetic and potential energies is linearly related to the gradient Richardson number.
Lan, Changxing, et al. "Turbulence Structures in the Very Stable Boundary Layer Under the Influence of Wind Profile Distortion." Journal of Geophysical Research. Atmospheres, vol. 127, no. 20, Oct. 2022. https://doi.org/10.1029/2022jd036565
Lan, Changxing, Liu, Heping, Katul, Gabriel G., Li, Dan, & Finn, Dennis (2022). Turbulence Structures in the Very Stable Boundary Layer Under the Influence of Wind Profile Distortion. Journal of Geophysical Research. Atmospheres, 127(20). https://doi.org/10.1029/2022jd036565
Lan, Changxing, Liu, Heping, Katul, Gabriel G., et al., "Turbulence Structures in the Very Stable Boundary Layer Under the Influence of Wind Profile Distortion," Journal of Geophysical Research. Atmospheres 127, no. 20 (2022), https://doi.org/10.1029/2022jd036565
@article{osti_2422012,
author = {Lan, Changxing and Liu, Heping and Katul, Gabriel G. and Li, Dan and Finn, Dennis},
title = {Turbulence Structures in the Very Stable Boundary Layer Under the Influence of Wind Profile Distortion},
annote = {Abstract In very stable boundary layers (VSBL), a “cocktail” of submeso motions routinely result in elevated mean wind speed maxima above the ground, acting as a new source of turbulence generation. This new source of turbulent kinetic energy enhances turbulent mixing and causes mean wind profile distortion (WPD). As a results, this transient distortion in the wind profile adjusts the classical log‐law. Addressing how WPD‐induced turbulence regulates flow structures, turbulent fluxes, and transitions in stability regimes across layers remains a challenge. Eddy covariance data measured at four levels on a 62‐m tower are employed to address these questions. It is shown that the WPD initiates large turbulent eddies that penetrate downward, leading to enhanced vertical mixing and comparable turbulent transport efficiencies across layers. As a consequence, turbulence intensity and fluxes are increased. As the WPD is intensified, turbulent fluxes and turbulent flux transport caused by large eddies are also enhanced, leading to a transition from very stable to weakly stable regimes. Due to the influence of WPD‐induced large eddies, the large‐eddy turbulent Prandtl number does not deviate appreciably from unity and the partitioning between turbulent kinetic and potential energies is linearly related to the gradient Richardson number.},
doi = {10.1029/2022jd036565},
url = {https://www.osti.gov/biblio/2422012},
journal = {Journal of Geophysical Research. Atmospheres},
issn = {ISSN 2169-897X},
number = {20},
volume = {127},
place = {United States},
publisher = {American Geophysical Union; Wiley},
year = {2022},
month = {10}}
Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, Vol. 454, Issue 1971https://doi.org/10.1098/rspa.1998.0193