Eady–Eliassen model

E549982

The Eady–Eliassen model is a foundational theoretical framework in atmospheric dynamics used to analyze baroclinic instability and the development of midlatitude weather systems.

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Predicate Object
instanceOf atmospheric dynamics model
baroclinic instability model
theoretical model
appliesTo midlatitude troposphere
synoptic-scale atmospheric motions
assumes Boussinesq approximation
adiabatic flow
constant vertical shear of the basic flow
f-plane approximation
inviscid flow
rigid lower boundary
rigid upper boundary
uniform static stability
basedOn quasi-geostrophic theory
category atmospheric science
geophysical fluid dynamics models
theoretical meteorology
describes energy conversion from mean flow to eddies
growth rate of baroclinic disturbances
tilt of eddies with height
vertical structure of unstable modes
field atmospheric dynamics
geophysical fluid dynamics
influenced development of modern baroclinic instability theory
involves boundary conditions at top and bottom of the atmosphere
eigenvalue problem for growth rates
normal-mode decomposition
provides characteristic horizontal wavelength of most unstable modes
maximum growth rate for baroclinic waves under idealized conditions
relatedTo Charney model of baroclinic instability NERFINISHED
Eady model NERFINISHED
Eliassen–Palm theory NERFINISHED
quasi-geostrophic potential vorticity equation
simplifies full primitive equations of motion
usedFor analysis of baroclinic instability
diagnosis of synoptic-scale disturbances
linear stability analysis of atmospheric flows
study of midlatitude weather systems
understanding growth of baroclinic waves
usedIn idealized numerical experiments of baroclinic waves
teaching of synoptic and dynamical meteorology
theoretical studies of cyclone development

Referenced by (1)

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Arnt Eliassen hasEponym Eady–Eliassen model