Incompressibility

From Glossary of Meteorology



incompressibility

An idealized condition in which compressibility vanishes.

Most liquids are nearly incompressible. For shallow layers of the atmosphere with velocity fluctuations much less than the speed of sound, incompressibility is a good approximation and is often made for mathematical convenience. For a fluid with a density depending on temperature, incompressibility does not imply non-divergence.
See anelastic approximation, Boussinesq approximation.


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.