Rossby number

E621609

The Rossby number is a dimensionless quantity in fluid dynamics and meteorology that compares inertial to Coriolis forces, indicating the importance of Earth's rotation in large-scale atmospheric and oceanic flows.

All labels observed (2)

Label Occurrences
Rossby number canonical 2
Rossby number is small 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf dimensionless quantity ⓘ
nondimensional number ⓘ
physical quantity ⓘ
appliesTo geostrophic flows ⓘ
large-scale atmospheric flows ⓘ
large-scale oceanic flows ⓘ
planetary-scale circulation ⓘ
synoptic-scale weather systems ⓘ
turbulent flows on a rotating planet ⓘ
category atmospheric dynamics concepts ⓘ
dimensionless numbers of fluid mechanics ⓘ
CoriolisParameterDefinition f = 2 Ω sin(φ) ⓘ
dependsOn latitude φ ⓘ
planetary rotation rate Ω ⓘ
describes relative importance of inertial forces to Coriolis forces ⓘ
dimensionless true ⓘ
field fluid dynamics ⓘ
geophysical fluid dynamics ⓘ
meteorology ⓘ
oceanography ⓘ
hasParameter Coriolis parameter f ⓘ
characteristic length scale L ⓘ
characteristic velocity U ⓘ
indicates importance of planetary rotation in a flow ⓘ
interpretation Ro ≈ 1 implies comparable inertial and Coriolis effects ⓘ
Ro ≪ 1 implies strong rotational control and near-geostrophic flow ⓘ
Ro ≫ 1 implies rotation is dynamically unimportant ⓘ
namedAfter Carl-Gustaf Rossby ⓘ
relatedTo Burger number ⓘ
Coriolis force ⓘ
Ekman number ⓘ
Froude number ⓘ
Reynolds number ⓘ
Rossby waves ⓘ
geostrophic balance ⓘ
inertial force ⓘ
scaleAssociation large Rossby number corresponds to small horizontal scales ⓘ
scaleAssociation small Rossby number corresponds to large horizontal scales ⓘ
symbol Ro ⓘ
typicalFormula Ro = U / (f L) ⓘ
typicalValueRange from much less than 1 to much greater than 1 depending on scale ⓘ
usedIn atmospheric dynamics ⓘ
climate modeling ⓘ
ocean circulation modeling ⓘ
rotating tank experiments ⓘ
weather forecasting ⓘ
usedToAssess importance of Coriolis terms in momentum equations ⓘ
validity of geostrophic approximation ⓘ
usedToClassify flow regimes in rotating fluids ⓘ

How these facts were elicited

Referenced by (3)

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

Coriolis effect → relatedConcept → Rossby number ⓘ
Carl-Gustaf Rossby → notableConcept → Rossby number ⓘ
Taylor–Proudman theorem → assumes → Rossby number is small ⓘ
linked to: Rossby number