turning latitude

From Glossary of Meteorology
The latitude below which the meridional structure of an equatorial gravity or Rossby wave is wavelike and beyond which the meridional structure is decaying.
With the β-plane approximation, the turning latitude (one in each hemisphere) is defined as
ams2001glos-Te49
where n is the meridional mode number, c is the phase speed of a given vertical mode Kelvin wave, and β is the derivative of Coriolis parameter f with respect to latitude.
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.