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Outflow boundary information


Outflow boundary on radar with radial velocity and frontal boundary drawn in.

An outflow boundary, also known as a gust front, is a storm-scale or mesoscale boundary separating thunderstorm-cooled air (outflow) from the surrounding air; similar in effect to a cold front, with passage marked by a wind shift and usually a drop in temperature and a related pressure jump. Outflow boundaries can persist for 24 hours or more after the thunderstorms that generated them dissipate, and can travel hundreds of kilometers from their area of origin. New thunderstorms often develop along outflow boundaries, especially near the point of intersection with another boundary (cold front, dry line, another outflow boundary, etc.). Outflow boundaries can be seen either as fine lines on weather radar imagery or else as arcs of low clouds on weather satellite imagery. From the ground, outflow boundaries can be co-located with the appearance of roll clouds and shelf clouds.[1]

Outflow boundaries create low-level wind shear which can be hazardous during aircraft takeoffs and landings. If a thunderstorm runs into an outflow boundary, the low-level wind shear from the boundary can cause thunderstorms to exhibit rotation at the base of the storm, at times causing tornadic activity. Strong versions of these features known as downbursts can be generated in environments of vertical wind shear and mid-level dry air. Microbursts have a diameter of influence less than 4 kilometres (2.5 mi), while macrobursts occur over a diameter greater than 4 kilometres (2.5 mi). Wet microbursts occur in atmospheres where the low levels are saturated, while dry microbursts occur in drier atmospheres from high-based thunderstorms. When an outflow boundary moves into a more stable low level environment, such as into a region of cooler air or over regions of cooler water temperatures out at sea, it can lead to the development of an undular bore.[2]

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  2. ^ Cite error: The named reference atkins was invoked but never defined (see the help page).

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Outflow boundary

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virtually no vertical wind shear weaken as soon as they send out an outflow boundary in all directions, which then quickly cuts off its inflow of relatively...

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dash labelled SQLN or squal line, while outflow boundaries are depicted as troughs with a label of outflow boundary. Fronts are the principal cause of significant...

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Wind shear

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three-dimensional boundary. The stronger the outflow boundary is, the stronger the resultant vertical wind shear will become. Weather fronts are boundaries between...

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ongoing by the time of these outlooks, focused along and north of an outflow boundary from Midland into northeastern Texas. The environment south of these...

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Downburst

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heat burst, is created by vertical currents on the backside of old outflow boundaries and squall lines where rainfall is lacking. Heat bursts generate significantly...

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Undular bore

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area of the atmosphere which is stable in the low levels after an outflow boundary or a cold front moves through. In hydraulics, an undular bore is a...

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Haboob

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thunderstorm Dust devil Intertropical Convergence Zone Khamsin Mistral (wind) Outflow boundary Simoom Sirocco Haboob at the Encyclopædia Britannica Farquharson, J...

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Mesoscale convective complex

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upper-troposphere. Near the surface, the MCC exhibits high pressure, with an outflow boundary, or mesoscale cold front, at its leading edge. This high pressure is...

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Wall cloud

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condensation from the cool outflow of the storm that lifts warmer air in the ambient environment (at the outflow boundary). When present in a supercell...

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OFB

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Football Association (German: Österreichischer Fußball-Bund, ÖFB) Outflow boundary, in meteorology, the leading edge of precipitation-cooled air emanating...

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1953 Waco tornado outbreak

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activity from the overnight hours persisted, generating residual outflow boundaries. Already, anomalously warm surface temperatures reached the mid-70s...

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Bow echo

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storm detection Derecho Gustnado Hook echo Mesoscale convective system Outflow boundary Rear-inflow jet Tornado Bow Echo Prototype Klimowski, Brian A.; Mark...

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Landspout

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boundary layer vorticity upward into a vertical axis and tightens it into a strong vortex. Landspouts can also occur due to interactions from outflow...

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regions around other thunderstorms. They may also be visible as an outflow boundary hours or days after convection and can pinpoint areas of favored thunderstorm...

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Frontolysis

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air masses diverge are called areas of frontolysis. Frontogenesis Outflow boundary Thralls, Zoe A. (1958). The Teaching of Geography. Appleton-Century-Crofts...

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March 1990 Central United States tornado outbreak

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the south of a quasi-stationary weather front, leaving a distinct outflow boundary across central and eastern Kansas. Early on March 13, morning atmospheric...

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Dry line

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resulting in convective clouds. Surface weather analysis Weather front Outflow boundary Scott Girhard (2007-05-04). "Lecture 3 - Thunderstorms". San Antonio...

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Tropical cyclogenesis

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Convergence Zone (ITCZ), a tropical wave, a broad surface front, or an outflow boundary, a low level feature with sufficient vorticity and convergence is required...

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