outflow velocity - significado y definición. Qué es outflow velocity
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Qué (quién) es outflow velocity - definición

AIR THAT FLOWS OUTWARDS FROM A STORM SYSTEM
Cirrus outflow; Upper-level outflow; Upper level outflow
  • The outflow boundary indicated by the presence of this shelf cloud preceded a [[derecho]] in [[Minnesota]]
  • Structure of a tropical cyclone. The upper level outflow is depicted by [[cirrus cloud]]s in the upper part of the schematic
  • Outflow boundary that preceded a strong thunderstorm in [[Oklahoma]]
  • Doppler radar station]]. The outflow produces a gust front that moves ahead of the main thunderstorm.

Detonation velocity         
CHARACTERISTIC OF EXPLOSIONS
Velocity of detonation; Detonation speed; Explosive velocity
Explosive velocity, also known as detonation velocity or velocity of detonation (VoD), is the velocity at which the shock wave front travels through a detonated explosive. Explosive velocities are always faster than the local speed of sound in the material.
Four-velocity         
ANALOGUE OF VELOCITY IN FOUR-DIMENSIONAL SPACETIME
Four velocity; Velocity Four-Vector; Velocity four-vector; 4-velocity; Four-speed; 4-speed
In physics, in particular in special relativity and general relativity, a four-velocity is a four-vector in four-dimensional spacetimeTechnically, the four-vector should be thought of as residing in the tangent space of a point in spacetime, spacetime itself being modeled as a smooth manifold. This distinction is significant in general relativity.
Ventricular outflow tract obstruction         
OCCLUSION OF THE OUTFLOW TRACT IN A VENTRICLE OF THE HEAR
Left ventricular outflow tract obstruction; Right ventricular outflow tract obstruction; RVOTO; LVOTO; Ventricular outflow obstruction
A ventricular outflow tract obstruction is one type of congenital heart defect in which either the right or left ventricular outflow tract is blocked or obstructed. These obstructions represent a spectrum of disorders.

Wikipedia

Outflow (meteorology)

Outflow, in meteorology, is air that flows outwards from a storm system. It is associated with ridging, or anticyclonic flow. In the low levels of the troposphere, outflow radiates from thunderstorms in the form of a wedge of rain-cooled air, which is visible as a thin rope-like cloud on weather satellite imagery or a fine line on weather radar imagery. For observers on the ground, a thunderstorm outflow boundary often approaches in otherwise clear skies as a low, thick cloud that brings with it a gust front.

Low-level outflow boundaries can disrupt the center of small tropical cyclones. However, outflow aloft is essential for the strengthening of a tropical cyclone. If this outflow is restricted or undercut, the tropical cyclone weakens. If two tropical cyclones are in close proximity, the upper-level outflow from the upwind system can limit the development of the other system.