Construct · 3 fields · 3 citations
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In fluid dynamics a jet is a narrow, fast stream of fluid issuing into a surrounding body of the same or another fluid, carrying momentum forward while entraining and mixing the ambient fluid along its edges, and often breaking up once it becomes unstable. Rayleigh's 1878 On the instability of jets analysed mathematically why a smooth stream of fluid develops growing disturbances and fragments. The referent is a collimated momentum-driven flow characterised by its centreline speed, width, and spreading rate, the same construct that, scaled up, becomes a current of air or a beam of cosmic plasma.[1]
In the atmosphere the same construct appears as the jet stream: a fast, narrow, meandering current of air near the tropopause, embedded in the broader flow and maintained by large-scale temperature and momentum gradients, that steers and energises midlatitude weather systems. Rossby's 1947 On the distribution of angular velocity in gaseous envelopes under the influence of large-scale horizontal mixing processes set out the dynamics concentrating westerly momentum into such a current. It is the identical collimated fast-flow idea as a laboratory jet, realised as a planetary wind and measured by its core wind speed, width, and position rather than by a nozzle flow.[2]
In astrophysics a jet is a highly collimated, often relativistic outflow of plasma launched from the vicinity of an accreting compact object such as a supermassive black hole, extending far beyond its host galaxy and feeding the lobes of radio sources. Blandford and Rees's 1974 A 'twin-exhaust' model for double radio sources proposed how a confined channel collimates such a flow into opposing beams. It is the same collimated momentum-carrying flow as a water jet or the jet stream, here made of magnetised plasma at cosmic scale and measured by its emission morphology and speed rather than by a flow meter.[3]
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