Turbulence

From Glossary of Meteorology
(Redirected from Atmospheric turbulence)



turbulence

  1. Irregular fluctuations occurring in fluid motions.

    It is characteristic of turbulence that the fluctuations occur in all three velocity components and are unpredictable in detail; however, statistically distinct properties of the turbulence can be identified and profitably analyzed. Turbulence exhibits a broad range of spatial and temporal scales resulting in efficient mixing of fluid properties. Analysis reveals that the kinetic energy of turbulence flows from the larger spatial scales to smaller and smaller scales and ultimately is transformed by molecular (viscous) dissipation to thermal energy. Therefore, to maintain turbulence, kinetic energy must be supplied at the larger scales.
    See also ocean mixing.

  2. Random and continuously changing air motions that are superposed on the mean motion of the air.


    Fleagle, R. G., and J. A. Businger 1980. An Introduction to Atmospheric Physics. 2d ed., Academic Press, . p. 264.

    Frisch, U. 1995. Turbulence: The Legacy of A. N. Kolmogorov. Cambridge University Press, . 1–22.

    Hinze, J. O. 1975. Turbulence. 2d ed., McGraw–Hill, . 790 pp.


Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.