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It is often used in [[atmospheric science]], particularly in the study of [[stratosphere|stratospheric]] dynamics. ...

{{short description|Ordinary differential equation used in the field of fluid dynamics}} ...Taylor–Goldstein equation is derived from the 2D [[Euler equations (fluid dynamics)|Euler equations]], using the [[Boussinesq approximation (buoyancy)|Boussin ...

...chlieren deflectometry for temperature analysis of filamentary non-thermal atmospheric pressure plasma|journal=Review of Scientific Instruments|date=2012|volume=8 ...|first5=K.-D.|title=On plasma parameters of a self-organized plasma jet at atmospheric pressure|journal=The European Physical Journal D|date=14 September 2010|vol ...

The '''atmospheric circulation on exoplanets''' refers to the large-scale movement of air mass ...tics, such as [[Rotational frequency|rotation rate]] (fast vs. slow) and [[atmospheric stratification]] (stable vs. unstable), influence circulation patterns. For ...

{{Short description|Quantity associated with atmospheric waves}} ...book |last1=Vallis |first1=Geoffrey K |title=Atmospheric and Oceanic Fluid Dynamics - Fundamentals and Large-scale Circulation |date=2006 |publisher=Cambridge ...

{{Short description|Coordinate system used in fluid dynamics}} ...ctions/technotes/asset-000-000-000-845.pdf|publisher=[[National Center for Atmospheric Research]]|accessdate=2011-01-03|author2=Gall, Robert|author3=Pyle, Matthew ...

'''Q-vectors''' are used in atmospheric dynamics to understand physical processes such as vertical motion and [[frontogenesi ...ated by the constant 1e⁻⁴ s⁻¹; <math>R</math> is the atmospheric [[ideal gas constant]]; <math> \beta </math> is the latitudinal change in t ...

* [[Cybernetics]]<ref>{{Cite web |title=Fuzzy differential inclusion in atmospheric and medical cybernetics |url=https://www.isibang.ac.in/~kaushik/kaushik_fil * [[Atmospheric dispersion modeling]] ...

The '''Eady model''' is an [[atmospheric model]] for [[baroclinic instability]] first posed by British meteorologist ...ble modes have height, [[vorticity]], vertical velocity, and several other atmospheric parameters with contours that tilt westward with height, though temperature ...

{{Short description|Dynamics of naturally occurring flows}} ...b|Model forecast of [[Hurricane Mitch]] created by the [[Geophysical Fluid Dynamics Laboratory]]. The arrows are wind vectors and the grey shading indicates an ...

Trajectories are useful for tracking atmospheric contaminants, such as smoke plumes, and as constituents to [[Lagrangian coo ...pherical Earth. The differential equations for tracing a two-dimensional, atmospheric trajectory in longitude-latitude coordinates are as follows: ...

...try equations''' are the [[equations of motion]] governing the unpowered [[Atmospheric entry|reentry]] of a [[spacecraft]], based on the assumptions of planar mot * <math>\rho</math> is the [[Density of air|atmospheric density]] ...

{{details|Boundary conditions in computational fluid dynamics}} ...set of constraints to [[boundary value problem]]s in [[computational fluid dynamics]]. These boundary conditions include inlet boundary conditions, outlet boun ...

..., are <ref name="vallis">Vallis, Geoffrey K. Atmospheric and oceanic fluid dynamics: fundamentals and large-scale circulation. Cambridge University Press, 2006 *[[Geophysical fluid dynamics]] ...

...st=Anderson, Jr. |first=John D. |title=Hypersonic and High-Temperature Gas Dynamics |publisher=American Institute of Aeronautics and Astronautics |year=2019 |i ...or estimating the severe aerodynamic heating conditions encountered during atmospheric entry and for designing appropriate thermal protection measures. ...

...omly in space and time. Models of continuous gusts are used to represent [[atmospheric turbulence]], especially [[clear air turbulence]] and turbulent winds in [[ ...and von Kármán models, are generally used for continuous gusts in [[flight dynamics]] applications.{{sfn|MIL-STD-1797A|1990|p=678}}{{sfn|Hoblit|1988|loc=Chap. ...

...of the atmosphere/oceanic dynamics,<ref>R. Camassa, On the geometry of an atmospheric slow manifold, ''Physica D'', '''84''':357&ndash;397, 1995.</ref> ...o be the invariant manifold on which the dynamics are slow compared to the dynamics off the manifold. The slow manifold in a particular problem would be a sub- ...

[[File:Many-layered atmospheric model.png|thumb|412x412px|A multi-layered model of the atmosphere is shown, ...quilibrium temperature]].<ref name=":0" /><ref name=":2">{{Cite book|title=Atmospheric Evolution on Inhabited and Lifeless Worlds|last=Catling|first=David C.|publ ...

...n |first3=M. |last4=Hasselmann |first4=K. |last5=Janssen |first5=P. |title=Dynamics and modelling of ocean waves |date=1996 |publisher=Cambridge University Pre ...positive energy flux. Using dimensional analysis, Jeffreys showed that the atmospheric pressure can be displayed as ...

...pical Cyclones. Part I: Steady-State Maintenance| journal = Journal of the Atmospheric Sciences| volume = 43| issue = 6| pages = 585–605| year = 1986| last1 = Ema ...e = Dissipative heating and hurricane intensity| journal = Meteorology and Atmospheric Physics| volume = 65| issue = 3–4| pages = 233–240| year = 1998| last1 = Bi ...