A squall is a sudden, sharp increase in wind speed which is usually associated with active weather, such as rain showers, thunderstorms, or heavy snow. [The Weather Channel. [http://www.weather.com/glossary/s.html Weather Glossary: S.] Retrieved on 2006-11-19.] Squalls refer to an increase in the sustained winds over a short time interval, as there may be higher gusts during a squall event. [Australian Bureau of Meteorology. [http://www.bom.gov.au/info/wwords/ Weather Words.] Retrieved on 2006-11-19.] They usually occur in a region of strong mid-level height falls,clarifyme|September 2008 or mid-level tropospheric cooling, which force strong localized upward motions at the leading edge of the region of cooling, which then enhances local downward motions just in its wake.
Origin of the term
The word appears to be Nordic in origin, but its
etymologyis considered obscure. It probably has its roots in the word "skvala" [ [http://www.answers.com/topic/squall?cat=technology squall: Definition and Much More from Answers.com ] ] an Old Norse word meaning literally, "to squeal". [Georoots News. [http://www.georoots.org/Georoots_News/Volume_1/georoots_v1_5.htm Georoots News V.1#5: Changes in the Wind.] Retrieved on 2006-12-30.] The first known use of the term on surface weather analyses was in the United Statesin the late Nineteenth Century on U. S. Signal Corp Maps, begun in 1871.
Character of the wind
The term "squall" is universally used to refer to a sudden wind-speed increase, both historically and in the present day. To be called a squall in the
United States, the wind must increase at least 18 miles per hour(8 meters per second) and must attain a top speed of at least 25 miles per hour (11 meters per second), lasting at least a full minute in duration. In Australia, a squall is defined to last for several minutes before the wind returns to the long term mean value. In either case, a squall is defined to last about half as long as the definition of sustained wind in its respective country. Usually, this sudden violent wind is associated with briefly heavy precipitation.
Known locally as pamperos, they are used to describe strong downsloped winds that move across the pampas, eventually making it to the
Atlantic Ocean. [Oxford English Dictionary. Oxford University Press. 10Rev Ed edition (7 April 2005)]
Central America, the term gully squall is used to describe strong increases of the wind forced through sharp mountain valleys on the Pacific Oceanside of the isthmus.
Bayamo is a term used to describe squalls emanating from tropical thunderstorms near the Bight of Bayamo. [WGN-TV. [http://wgntv.trb.com/news/weather/wgntv-weatherwords-b,0,1454739.story?coll=wgntv-weather-4 Weather Words - B.] Retrieved on 2006-11-19.]
East Indies, brubu is a name for a squall [ [http://ggweather.com/winds.html Wind Names ] ]
Pacific Northwest - United States
Pacific Northwest, a squall is a short but furious rainstorm with strong winds, often small in area and moving at high speed, especially as a maritime term. Such a strong outflow occurring in fjords and inlets is referred to by mariners as a squamish.
Bull's Eye Squall is a term used offshore South Africa, describing a squall forming in fair weather. It is named for the appearance of the small isolated cloud marking the top of the squall.Golden Gate Weather Services. [http://ggweather.com/winds.html Names of Winds.] ]
Philippines [West Pacific]
In most parts of the country, squalls are called subasko characterized by heavy rains driven by blustery winds. Local fishermen at sea are often on the lookout for signs of impending squalls on the open water and rush to shore at its early early hints.
A squall line is an organized line of
thunderstorms. It is classified as a multi-cell cluster, meaning a thunderstorm complex comprising many individual updrafts. They are also called multi-cell lines. Squalls are sometimes associated with hurricanes or other cyclones, but they can also occur independently. Most commonly, independent squalls occur along front lines, and may contain heavy precipitation, hail, frequent lightning, dangerous straight line winds, and possibly funnel clouds, tornadoes and waterspouts. [Weatherquestions.com. [http://www.weatherquestions.com/What_is_a_squall_line.htm What is a Squall Line?] Retrieved on 2006-11-19.] Squall lines require significant low-level warmth and humidity, a nearby frontal zone, and vertical wind shear from an angle behind the frontal boundary. [Wilfried Jacobs. [http://www.zamg.ac.at/eumetrain/EUMeTrain2005/Squall/intro.htm EUMeTrain: Case Study on Squall Line.] Retrieved on 2006-11-19.] The strong winds at the surface are usually a reflection of dry air intruding into the line of storms, which when saturated, falls quickly to ground level due to its much higher density before it spreads out downwind. [Thinkquest. [http://library.thinkquest.org/C0112425/stu_thundertornado.htm#2 Meteorology Online: Squall.] Retrieved on 2006-11-19.] In England, a squall associated with tempestuous weather is known as a blunk. Significant squall lines with multiple bow echoes are known as derechos. [Robert H. Johns and Jeffry S. Evans. Storm Prediction Center. [http://www.spc.ncep.noaa.gov/misc/AbtDerechos/derechofacts.htm Derecho Facts.] Retrieved on 2006-11-19.]
quall Line Life Cycle
There are several forms of
mesoscale meteorology, including simplistic isolated thunderstorms unrelated to advancing cold fronts, to the more complex daytime/nocturnal Mesoscale Convective System(MCS) and Mesoscale Convective Complex(MCC), to squall linethunderstorms.
quall Line Formation
The main driving force behind squall line creation is attributed to the process of in-filling of multiple thunderstorms and/or a single area of thunderstorms expanding outward within the leading space of an advancing
The leading area of a squall line is composed primarily of multiple updrafts, or singular regions of an
updraft, rising from ground level to the highest extend of the troposhere, condensing water and building a dark, ominous clouds to one with a noticeable overshooting top and anvil (thanks to synoptic scale winds). Because of the chaotic nature of updrafts and downdrafts, pressure perturbations are important.
Pressure perturbations within an extent of a thunderstorm are noteworthy. With
buoyancyrapid within the lower and mid-levels of a mature thunderstorm, one might believe that low pressure dominates in the mesoscale environment. However, this is not the case. With downdrafts ushering colder air from mid-levels, hitting ground and propagating away in all directions, high pressure is to be found widely at surface levels, usually indicative of strong (potentially damaging winds).
shearis an important aspect to measuring the potential of squall line severity and duration. In low to medium shear environments, mature thunderstorms will contribute modest amounts of downdrafts, enough to turn will aid in create a leading edge lifting mechanism - the gust front. In high shear environments created by opposing low level jet winds and synoptic winds, updrafts and consequential downdrafts can be much more intense (common in supercell mesocyclones). The cold air outflowleaves the trailing area of the squall line to the mid-level jet, which aids in downdraft processes.
quall Line Evolution
As thunderstorms fill into a distinct line, strong leading-edge updrafts - occasionally visible to a ground observer in the form of a
shelf cloud, appear as an ominous sign of potential severe weather.
Beyond the strong winds because of updraft/downdraft behavior, heavy rain (and
hail) is another sign of a squall line. In the winter, squall lines can occur albeit less frequently - bringing heavy snowand/or thunderand lightning - usually over inland lakes(i.e. Great Lakesregion).
Following the initial passage of a squall line, light to moderate
stratiformprecipitation is also common. A Bow echois frequently seen on the northern and southern most reaches of squall line thunderstorms (via satellite imagery. This is where the northern and southern ends curl backwards towards the middle portions of the squall line, making a "bow" shape. Bow echoes are frequently featured within supercellmesoscale systems.
The northern end of the squall line is commonly referred to as the cyclonic end, with the southern side rotating anticyclonically. Because of the
coriolis force, the northern end may evolve further, creating a "comma shaped" mesolow, or may continue in a squall-like pattern.
quall Line Dissipation
As supercell or multi-cell thunderstorms disappate because of a weak shear, poor lifting mechanisms: (e.g. considerable
terrainor lack of daytime heating. The squall lineassociated gust frontmay outrun the squall line, the synoptic scale low may fill - leading to a weaking of a cold front, or the thunderstorm has exhausted its updrafts, becoming purely a downdraft dominated system. The areas of disappating squall line thunderstorms may be regions of low CAPE, low humidity, insufficient wind shear, or poor synoptic dynamics (e.g. an upper level low filling) leading to frontolysis.
From here, a general thinning of a squall line will occur: within, winds decaying with time, outflow boundaries weakening updrafts substantially, and clouds losing their thickness.
igns in the sky
Shelf clouds and roll clouds are usually seen above the leading edge of a squall, also known as a
thunderstorm's gust front. [National Weather Service Forecast Office, Springfield, Missouri. [http://www.crh.noaa.gov/sgf/?n=spotter_squall_lines Storm Spotter Online Training.] Retrieved on 2006-11-19.] From the time these low cloud features appear in the sky, one can expect a sudden increase in the wind in less than 15 minutes.
Tropical cyclones normally have squalls coincident with spiral bands of greater curvature than many mid-latitude systems due to their smaller size. This squalls can harbor waterspoutsand tornadoesdue to the significant vertical wind shearwhich exists in the vicinity of a tropical cyclone's outer bands.
Snow squallscan be spawned by an intrusion of cold air aloft over a relatively warm surface layer. Lake effect snows can be in the form of a snow squall. In Scotland, snow squalls are known as bluffarts.
Squall is a vocabulary word in the book "
Sarah, Plain and Tall" in the title of the book "White Squall", written by John Conroy Hutcheson in 1900. [Athelstane E-Books. [http://www.athelstane.co.uk/jc_hutch/whisqual/about.htm John Conroy Hutcheson.] Retrieved on 2006-11-19.]
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