Charney–Eliassen model

E542053

The Charney–Eliassen model is a foundational quasi-geostrophic framework in atmospheric dynamics used to describe large-scale, balanced motions such as midlatitude cyclones and jet streams.

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Charney–Eliassen model canonical 1

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Statements (46)

Predicate Object
instanceOf atmospheric dynamics model ⓘ
quasi-geostrophic model ⓘ
theoretical framework ⓘ
appliesTo midlatitudes ⓘ
synoptic-scale atmospheric motions ⓘ
assumes geostrophic balance ⓘ
hydrostatic balance ⓘ
small Rossby number ⓘ
small perturbations about a basic state ⓘ
basedOn quasi-geostrophic approximation ⓘ
basicState thermal wind balanced jet ⓘ
zonal mean flow ⓘ
category balanced atmospheric models ⓘ
large-scale circulation models ⓘ
coreConcept potential vorticity conservation ⓘ
thermal wind balance ⓘ
thermodynamic energy equation ⓘ
vorticity equation ⓘ
describes jet streams ⓘ
large-scale balanced atmospheric motions ⓘ
midlatitude cyclones ⓘ
field atmospheric dynamics ⓘ
geophysical fluid dynamics ⓘ
historicalRole foundational framework in synoptic-scale meteorology ⓘ
mathematicalForm elliptic partial differential equation for streamfunction ⓘ
set of linearized quasi-geostrophic equations ⓘ
namedAfter Arnt Eliassen ⓘ
Jule Gregory Charney ⓘ
neglects ageostrophic inertia-gravity waves ⓘ
small-scale turbulence ⓘ
relatedTo Rossby waves ⓘ
baroclinic instability theory ⓘ
quasi-geostrophic theory ⓘ
scale synoptic scale ⓘ
spatialScale thousands of kilometers ⓘ
timeScale days ⓘ
usedFor analyzing jet stream dynamics ⓘ
balanced flow analysis ⓘ
diagnosing secondary circulations ⓘ
idealized studies of midlatitude cyclones ⓘ
studying baroclinic development ⓘ
usedIn idealized numerical experiments ⓘ
theoretical meteorology education ⓘ
uses pressure coordinates ⓘ
streamfunction formulation ⓘ
validUnder large-scale slowly varying flow conditions ⓘ

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Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Jule Gregory Charney → knownFor → Charney–Eliassen model ⓘ