Author Archives: Michael Fagin

14 Jul

Frontal Squall Lines

General Info, Poor Visibility, Turbulence, Weather ConditionsComments are off

Frontal squall lines form just ahead of surface cold fronts and dry lines, and also ahead of upper-level fronts. If the necessary conditions exist, they may stretch to hundreds of miles in length. They may bring tornadoes and hail but they’re more commonly associated with strong straight-line winds. If the flow along a squall line

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15 Jun

Hook Echoes- Unstable Air Mass

General Info, Lightning, Weather ConditionsComments are off

Hook echoes are meteorological phenomena named after their shapes. They’re created when vertical wind shear causes warm, moist air, sucked in by the unstable movements of a supercell thunderstorm, to mix with a different incoming channel of drier, cooler air. The shape they assume resembles a hook because the two streams of air aren’t mixing

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19 Apr

Hazard of ice crystals

Icing on WingsWith 0 comments

Clouds at temperatures between 0 and -40C contain a mixture of ice crystals and super-cooled water. At colder temperatures, ice crystals prevail. Super-cooled water is responsible for the threat of aircraft structural icing, but at lower temperatures, this threat decreases. Because of the lack of super-cooled water, icing, other that of light intensity, is unlikely

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17 Apr

Microburst

MicroburstWith 0 comments

A microburst is a strong downward oriented wind usually associated with thunderstorms. These winds usually form within a cumulonimbus cloud that is mature and are often associated with heavy rain and perhaps along with hail. These winds can cause major issues such as crashes with airplanes during take-off and or landing. In an attempt to

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