About: Denver Convergence Vorticity Zone

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The Denver Convergence Vorticity Zone (DCVZ) is an orographically-induced atmospheric phenomenon characterized by convergent winds in the High Plains just east of the Denver metropolitan area, typically 50 to 100 km (30 to 60 mi) in length and oriented in a north-south direction. This meteorological feature was subject to scientific scrutiny following a large outbreak of Denver-area tornadoes in 1981 and is implicated in the propensity of the area to spawn landspout (misocyclone) and supercell (mesocyclone) tornadoes. The DCVZ is often associated with the effect, which some consider as a more fully developed iteration of the DCVZ, although the Denver Cyclone is considered a distinct atmospheric phenomenon by some scientists.

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  • The Denver Convergence Vorticity Zone (DCVZ) is an orographically-induced atmospheric phenomenon characterized by convergent winds in the High Plains just east of the Denver metropolitan area, typically 50 to 100 km (30 to 60 mi) in length and oriented in a north-south direction. This meteorological feature was subject to scientific scrutiny following a large outbreak of Denver-area tornadoes in 1981 and is implicated in the propensity of the area to spawn landspout (misocyclone) and supercell (mesocyclone) tornadoes. The DCVZ is often associated with the effect, which some consider as a more fully developed iteration of the DCVZ, although the Denver Cyclone is considered a distinct atmospheric phenomenon by some scientists. (en)
  • 丹佛輻合渦度帶（英語：Denver Convergence Vorticity Zone，縮寫：DCVZ）是一條在丹佛市郡以東形成的輻合帶，長度約50至100公里，為南北走向。此一現象在1981年丹佛地區大規模爆發龍捲風而被提出。此現象被用以解釋該地區容易產生噴流與龍捲風，儘管有一部份科學家認為丹佛輻合渦度帶是一種獨特的天氣現象，但仍被認為其與丹佛氣旋效應有關。 (zh)
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  • January 2018 (en)
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  • The Denver Convergence Vorticity Zone (DCVZ) is an orographically-induced atmospheric phenomenon characterized by convergent winds in the High Plains just east of the Denver metropolitan area, typically 50 to 100 km (30 to 60 mi) in length and oriented in a north-south direction. This meteorological feature was subject to scientific scrutiny following a large outbreak of Denver-area tornadoes in 1981 and is implicated in the propensity of the area to spawn landspout (misocyclone) and supercell (mesocyclone) tornadoes. The DCVZ is often associated with the effect, which some consider as a more fully developed iteration of the DCVZ, although the Denver Cyclone is considered a distinct atmospheric phenomenon by some scientists. (en)
  • 丹佛輻合渦度帶（英語：Denver Convergence Vorticity Zone，縮寫：DCVZ）是一條在丹佛市郡以東形成的輻合帶，長度約50至100公里，為南北走向。此一現象在1981年丹佛地區大規模爆發龍捲風而被提出。此現象被用以解釋該地區容易產生噴流與龍捲風，儘管有一部份科學家認為丹佛輻合渦度帶是一種獨特的天氣現象，但仍被認為其與丹佛氣旋效應有關。 (zh)
rdfs:label
  • Denver Convergence Vorticity Zone (en)
  • 丹佛輻合渦度帶 (zh)
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