The Spanish Plume (Penacho Ibérico in Spanish and Spaanse Pluim in Dutch) is a weather pattern in which a plume of warm air moves from the Iberian plateau or the Sahara to northwestern Europe, causing thunderstorms. This meteorological pattern can lead to extreme high temperatures and intense rainfall during the summer months, with potential for flash flooding, damaging hail, and tornado formation. Some of these intense thunderstorms are formed from thermal lows, which are also known as heat lows. Thermal lows can be semipermanent features around some parts of Europe, particularly in the summer season. These thermal lows can be developed or created around Spain, Portugal, France etc., during the summer season because of the intense heat. Thermal low pressure can be located around the world
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| - Penacho ibérico (es)
- Spaanse pluim (nl)
- Spanish plume (en)
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| - El penacho ibérico (The Spanish plume en fuentes en inglés) es un patrón sinóptico en Europa occidental que consiste en la advección hacia latitudes superiores de una lengua de aire cálido de niveles bajos desde zonas como la meseta de la península ibérica yendo por delante de una vaguada de aire frío en niveles altos. Este patrón meteorológico puede dar lugar a episodios de lluvias torrenciales, elevadas temperaturas y tormentas con granizo en las islas británicas y el noroeste de Europa e incluso tornados durante los meses de verano en lugares como Alemania. (es)
- De Spaanse pluim (penacho ibérico in het Spaans, Spanish plume in het Engels) is een natuurverschijnsel waarin zeer warme en droge lucht vanuit het Iberisch Schiereiland in pluimvorm richting Noordwest-Europa wordt gestuwd. De warme lucht vormt een soort deken bovenop koelere luchtlagen, waardoor zeer broeierig weer ontstaat. In de zomermaanden kan dit leiden tot zware regen- en hagelbuien, onweer en tornadovorming. (nl)
- The Spanish Plume (Penacho Ibérico in Spanish and Spaanse Pluim in Dutch) is a weather pattern in which a plume of warm air moves from the Iberian plateau or the Sahara to northwestern Europe, causing thunderstorms. This meteorological pattern can lead to extreme high temperatures and intense rainfall during the summer months, with potential for flash flooding, damaging hail, and tornado formation. Some of these intense thunderstorms are formed from thermal lows, which are also known as heat lows. Thermal lows can be semipermanent features around some parts of Europe, particularly in the summer season. These thermal lows can be developed or created around Spain, Portugal, France etc., during the summer season because of the intense heat. Thermal low pressure can be located around the world (en)
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| - El penacho ibérico (The Spanish plume en fuentes en inglés) es un patrón sinóptico en Europa occidental que consiste en la advección hacia latitudes superiores de una lengua de aire cálido de niveles bajos desde zonas como la meseta de la península ibérica yendo por delante de una vaguada de aire frío en niveles altos. Este patrón meteorológico puede dar lugar a episodios de lluvias torrenciales, elevadas temperaturas y tormentas con granizo en las islas británicas y el noroeste de Europa e incluso tornados durante los meses de verano en lugares como Alemania. (es)
- The Spanish Plume (Penacho Ibérico in Spanish and Spaanse Pluim in Dutch) is a weather pattern in which a plume of warm air moves from the Iberian plateau or the Sahara to northwestern Europe, causing thunderstorms. This meteorological pattern can lead to extreme high temperatures and intense rainfall during the summer months, with potential for flash flooding, damaging hail, and tornado formation. Some of these intense thunderstorms are formed from thermal lows, which are also known as heat lows. Thermal lows can be semipermanent features around some parts of Europe, particularly in the summer season. These thermal lows can be developed or created around Spain, Portugal, France etc., during the summer season because of the intense heat. Thermal low pressure can be located around the world, particularly in the summer or in tropical regions. (en)
- De Spaanse pluim (penacho ibérico in het Spaans, Spanish plume in het Engels) is een natuurverschijnsel waarin zeer warme en droge lucht vanuit het Iberisch Schiereiland in pluimvorm richting Noordwest-Europa wordt gestuwd. De warme lucht vormt een soort deken bovenop koelere luchtlagen, waardoor zeer broeierig weer ontstaat. In de zomermaanden kan dit leiden tot zware regen- en hagelbuien, onweer en tornadovorming. (nl)
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