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Linha de instabilidade Linia szkwału Squall line Cóch líne スコールライン 飑线 Buienlijn Linea di groppo Bylinje
rdfs:comment
Líne chaol stoirmeacha toirní, a fhéadfaidh a bheith chomh fada leis na céadta ciliméadar, os comhair fronta fhuair, bíodh is nach mbíonn sí ach cúpla ciliméadar ar leithead. Baineann stoirmeacha toirní, anfaí is titim thobann teochta léi. スコールライン (squall line) とは、気象用語のひとつ。線状の活発な深い湿潤対流で、しばしば雷と、連続した降水域か、連続した降水域を含む破線状の降水域または破面状の降水域 かを伴う。スコールラインは、メソスケール対流システムの一種であって、スコールライン以外とは長さと幅との比によって区別される。 日本語では、西暦2000年頃まで陣風線(じんぷうせん)とも呼ばれてきたが、現在ではスコールラインと表記することが一般的。スコールラインは不安定線(ふあんていせん)に包含される現象。長さと幅との比であるが、一般的に幅30~40km程度で、長さが400~500km 程度のものをスコールラインと呼ぶが、日本ではこれよりも小規模な、幅20~50km程度で、長さが50~200km 程度のものもスコールラインと呼ぶ。また、日本では破面状の降水域を伴うものをスコールラインと呼ぶことは稀である。 En bylinje är välutvecklade åskväder som förekommer i linje, ofta knutna till en kallfront. Denna artikel om meteorologi eller klimatologi saknar väsentlig information. Du kan hjälpa till genom att lägga till den. A squall line, or more accurately a quasi-linear convective system (QLCS), is a line of thunderstorms, often forming along or ahead of a cold front. In the early 20th century, the term was used as a synonym for cold front (which often are accompanied by abrupt and gusty wind shifts). Linear thunderstorm structures often contain heavy precipitation, hail, frequent lightning, strong straight-line winds, and occasionally tornadoes or waterspouts. Particularly strong straight-line winds can occur where the linear structure forms into the shape of a bow echo. Tornadoes can occur along waves within a line echo wave pattern (LEWP), where mesoscale low-pressure areas are present. Some bow echoes can grow to become derechos as they move swiftly across a large area. On the back edge of the rainband Een buienlijn is een lijn van zware buien en/of onweersbuien. Vaak bevatten deze veel regen en onweer, terwijl er ook sterk veranderlijke zware windstoten op kunnen treden en soms ook hagel. De lijn kan een koufront, trog of ander systeem in de zijn. Doordat buienlijnen zich snel kunnen ontwikkelen en gepaard kunnen gaan met windstoten van meer dan 100 km/h en scherpe , kunnen ze zeer verraderlijk zijn. Ze komen veel voor in de intertropische convergentiezone en de tropische golf. Buienwolken kunnen hoogtes bereiken van meer dan 15 kilometer, waarbij de top uitwaaiert in de vorm van een aambeeld. In meteorologia con linea di groppo o linea dei groppi (in inglese squall line) s'intende una stretta e lunga fascia di temporali con un continuo e ben sviluppato fronte di raffica (gust front) sul bordo principale della linea. Tipica di fronti freddi, depressioni, tempeste e cicloni tropicali a medio-basse latitudini, la loro formazione è prerogativa del passaggio di un fronte freddo nei mesi più caldi dell'anno anche se non è da escludere una sua nascita durante il passaggio di un fronte freddo particolarmente intenso anche nei mesi autunnali o invernali. 准线形对流系统(英語:quasi-linear convective system),也称飑线(英語:Squall line),有时亦称线飑,是指带状的雷暴群所构成的风向、风速突变的一种中至小尺度的,通常伴随或先于冷锋出现。其破坏性很强大。飑线的产生多是由于行进至暖湿地区时造成了上冷下暖的格局,使对流层上下热力结构不同,产生高强度的强对流天气。飑线上的雷暴通常是由若干个雷暴单体组成的,因此可以产生剧烈的天气变化。在20世纪早期,飑线通常被用作冷锋的代名词。飑线过境时的典型现象为风向突变、风速快速增加、气压骤然上升以及气温急剧变化,全盛阶段平均风力在10级以上,阵风超过12级。同时也可能伴有雷暴、暴雨、冰雹、強力的直線風、龙卷风和海龍捲風。飑线通常具有典型的,並伴隨強力的直線風。龍捲風則可能在中尺度低壓區存在時沿著存在。在夏季時弓形回波可能會發展為,並以極高的速度通過大範圍區域。的後方邊緣通常伴隨著發展成熟的飑线,並存在,有時甚至伴隨熱暴流。飑线的水平范围很小,长度通常只有150~300公里,宽度仅半公里到几十公里,高度約10公里左右。其维持时间一般为4~10个小时。 Linia szkwału – strefa układających się w linię burz, które mają wspólną przyczynę powstania i formują się zwykle przed frontem chłodnym. Tego typu burze mogą tworzyć linie długości kilkuset kilometrów, często istnieją przez wiele godzin i mogą przynosić wiele wyładowań atmosferycznych, porywiste wiatry, intensywne opady deszczu i gradu, a czasem również tornada. Linha de instabilidade é uma zona de instabilidade na qual uma série de tempestades estão dispostas de forma alinhada. São tidas como uma tempestade multicelular, uma vez que são formadas por várias células convectivas de curta duração. A normalmente é mais intensa do que de tempestades de uma única célula, especialmente na direção do seu movimento frontal. Formam-se principalmente em regiões mais quentes, nas zonas tropicais. Sua ocorrência normalmente está associada a eventos de tempo severo, como chuva intensa, granizo, ventos fortes e até mesmo a formação de tornados. Podem ainda dar origem a um tipo de tempestade, o derecho, caracterizada por fortes ventos que atingem grandes áreas.
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Satellite image of storm line into Gulf of Mexico Radar image of a line of strong storms Radar image of eastern United States showing squall line
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dbo:abstract
A squall line, or more accurately a quasi-linear convective system (QLCS), is a line of thunderstorms, often forming along or ahead of a cold front. In the early 20th century, the term was used as a synonym for cold front (which often are accompanied by abrupt and gusty wind shifts). Linear thunderstorm structures often contain heavy precipitation, hail, frequent lightning, strong straight-line winds, and occasionally tornadoes or waterspouts. Particularly strong straight-line winds can occur where the linear structure forms into the shape of a bow echo. Tornadoes can occur along waves within a line echo wave pattern (LEWP), where mesoscale low-pressure areas are present. Some bow echoes can grow to become derechos as they move swiftly across a large area. On the back edge of the rainband associated with mature squall lines, a wake low can be present, on very rare occasions associated with a heat burst. Linia szkwału – strefa układających się w linię burz, które mają wspólną przyczynę powstania i formują się zwykle przed frontem chłodnym. Tego typu burze mogą tworzyć linie długości kilkuset kilometrów, często istnieją przez wiele godzin i mogą przynosić wiele wyładowań atmosferycznych, porywiste wiatry, intensywne opady deszczu i gradu, a czasem również tornada. En bylinje är välutvecklade åskväder som förekommer i linje, ofta knutna till en kallfront. Denna artikel om meteorologi eller klimatologi saknar väsentlig information. Du kan hjälpa till genom att lägga till den. Líne chaol stoirmeacha toirní, a fhéadfaidh a bheith chomh fada leis na céadta ciliméadar, os comhair fronta fhuair, bíodh is nach mbíonn sí ach cúpla ciliméadar ar leithead. Baineann stoirmeacha toirní, anfaí is titim thobann teochta léi. 准线形对流系统(英語:quasi-linear convective system),也称飑线(英語:Squall line),有时亦称线飑,是指带状的雷暴群所构成的风向、风速突变的一种中至小尺度的,通常伴随或先于冷锋出现。其破坏性很强大。飑线的产生多是由于行进至暖湿地区时造成了上冷下暖的格局,使对流层上下热力结构不同,产生高强度的强对流天气。飑线上的雷暴通常是由若干个雷暴单体组成的,因此可以产生剧烈的天气变化。在20世纪早期,飑线通常被用作冷锋的代名词。飑线过境时的典型现象为风向突变、风速快速增加、气压骤然上升以及气温急剧变化,全盛阶段平均风力在10级以上,阵风超过12级。同时也可能伴有雷暴、暴雨、冰雹、強力的直線風、龙卷风和海龍捲風。飑线通常具有典型的,並伴隨強力的直線風。龍捲風則可能在中尺度低壓區存在時沿著存在。在夏季時弓形回波可能會發展為,並以極高的速度通過大範圍區域。的後方邊緣通常伴隨著發展成熟的飑线,並存在,有時甚至伴隨熱暴流。飑线的水平范围很小,长度通常只有150~300公里,宽度仅半公里到几十公里,高度約10公里左右。其维持时间一般为4~10个小时。 Een buienlijn is een lijn van zware buien en/of onweersbuien. Vaak bevatten deze veel regen en onweer, terwijl er ook sterk veranderlijke zware windstoten op kunnen treden en soms ook hagel. De lijn kan een koufront, trog of ander systeem in de zijn. Doordat buienlijnen zich snel kunnen ontwikkelen en gepaard kunnen gaan met windstoten van meer dan 100 km/h en scherpe , kunnen ze zeer verraderlijk zijn. Ze komen veel voor in de intertropische convergentiezone en de tropische golf. Buienwolken kunnen hoogtes bereiken van meer dan 15 kilometer, waarbij de top uitwaaiert in de vorm van een aambeeld. Buienwolken ontstaan in gebieden waar warme lucht door convergentie sterk stijgt. Ze onderscheiden zich daarbij van luchtmassabuien door een duidelijke verticale windschering. De wind neemt daarbij sterk toe met de hoogte, waardoor er naast de stijgende warme lucht ook dalende koude luchtstromen kunnen voorkomen. Daardoor kunnen zichzelf veel langer in stand houden dan luchtmassabuien. Door de koude dalende luchtstromen ontstaat bij het aardoppervlak een meso-koufront dat steeds verder voor de bui uit kan gaan lopen, vaak met een rolwolk, soms met een stofstorm. Achter dit front kan de temperatuur sterk dalen en kunnen scherpe windsprongen optreden. Linha de instabilidade é uma zona de instabilidade na qual uma série de tempestades estão dispostas de forma alinhada. São tidas como uma tempestade multicelular, uma vez que são formadas por várias células convectivas de curta duração. A normalmente é mais intensa do que de tempestades de uma única célula, especialmente na direção do seu movimento frontal. Formam-se principalmente em regiões mais quentes, nas zonas tropicais. Sua ocorrência normalmente está associada a eventos de tempo severo, como chuva intensa, granizo, ventos fortes e até mesmo a formação de tornados. Podem ainda dar origem a um tipo de tempestade, o derecho, caracterizada por fortes ventos que atingem grandes áreas. In meteorologia con linea di groppo o linea dei groppi (in inglese squall line) s'intende una stretta e lunga fascia di temporali con un continuo e ben sviluppato fronte di raffica (gust front) sul bordo principale della linea. Tipica di fronti freddi, depressioni, tempeste e cicloni tropicali a medio-basse latitudini, la loro formazione è prerogativa del passaggio di un fronte freddo nei mesi più caldi dell'anno anche se non è da escludere una sua nascita durante il passaggio di un fronte freddo particolarmente intenso anche nei mesi autunnali o invernali. スコールライン (squall line) とは、気象用語のひとつ。線状の活発な深い湿潤対流で、しばしば雷と、連続した降水域か、連続した降水域を含む破線状の降水域または破面状の降水域 かを伴う。スコールラインは、メソスケール対流システムの一種であって、スコールライン以外とは長さと幅との比によって区別される。 日本語では、西暦2000年頃まで陣風線(じんぷうせん)とも呼ばれてきたが、現在ではスコールラインと表記することが一般的。スコールラインは不安定線(ふあんていせん)に包含される現象。長さと幅との比であるが、一般的に幅30~40km程度で、長さが400~500km 程度のものをスコールラインと呼ぶが、日本ではこれよりも小規模な、幅20~50km程度で、長さが50~200km 程度のものもスコールラインと呼ぶ。また、日本では破面状の降水域を伴うものをスコールラインと呼ぶことは稀である。
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