Gradient richardson number

From Glossary of Meteorology



gradient Richardson number

A dimensionless ratio, Ri, related to the buoyant production or consumption of turbulence divided by the shear production of turbulence.

It is used to indicate dynamic stability and the formation of turbulence:
ams2001glos-Ge35
where θv is virtual potential temperature, Tv is virtual absolute temperature, z is height, g is gravitational acceleration, and (U, V) are the wind components toward the east and north. The critical Richardson number, Ric, is about 0.25 (although reported values have ranged from roughly 0.2 to 1.0), and flow is dynamically unstable and turbulent when Ri < Ric. Such turbulence happens either when the wind shear is great enough to overpower any stabilizing buoyant forces (numerator is positive), or when there is static instability (numerator is negative).
Compare bulk Richardson number, flux Richardson number, Froude number.

Term edited 24 August 2023.


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.