wave theory of cyclogenesis
teoría ondulatoria de la ciclogénesis
cyclogenesis oor Spaans
cyclogenesis
en
(meteorology) the process which leads to the formation of tropical storms, cyclones and hurricanes; typically involves an interaction that leads to vertical wind shear
Vertalings in die woordeboek Engels - Spaans
ciclogénesis
en
the process which leads to the formation of tropical storms, cyclones and hurricanes
Ciclogénesis
Geskatte vertalings
Vertoon algoritmies gegenereerde vertalings
Soortgelyke frases
voorbeelde
Advanced filtering
Voorbeelde moet herlaai word.
Low upper-level wind shear and well-defined outflow contributed to further intensification, and the depression strengthened on August 10, despite being located in the eastern Caribbean Sea, which is an area not particularly suited to tropical cyclogenesis.
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Due to this direction of movement, African eastern waves are impelled along the southern periphery of the Azores High away from coastal West Africa towards the Caribbean, Central America, or the Bahamas, favouring tropical cyclogenesis, especially during the hurricane season.
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This generates favorable conditions for cyclogenesis in the upper atmosphere, which promotes the formation of an eastward-moving extratropical depression.
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The impact of dust clouds in the Atlantic, Caribbean and Gulf of Mexico on rainfall and tropical cyclogenesis was assessed and an extensive study was made of the effects of these clouds on human health
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As opposed to mid-latitude cyclogenesis, tropical cyclogenesis is driven by strong convection organised into a central core with no baroclinic zones, or fronts, extending through their center.
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After this process occurs, the growth period of the cyclone, or cyclogenesis, ends, and the low begins to spin down (fill) as more air is converging into the bottom of the cyclone than is being removed out the top since upper-level divergence has decreased.
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Tracking generally westward, environmental conditions favored tropical cyclogenesis and the system developed into a tropical depression the following day.
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The semi–permanent South Atlantic High influences its climate throughout the year by bringing in moist winds from the northeast, which bring most of the precipitation to the city in the form of frontal systems during winter or storms produced by cyclogenesis in autumn and winter.
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Occasionally, cyclogenesis will re-occur with occluded cyclones.
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The impact of dust clouds in the Atlantic, Caribbean and Gulf of Mexico on rainfall and tropical cyclogenesis was assessed and an extensive study was made of the effects of these clouds on human health.
Gracias, RojoUN-2 UN-2
On December 16, an extratropical cyclone over the Northern Pacific Ocean began showing signs of tropical cyclogenesis.
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Extratropical cyclones form anywhere within the extratropical regions of the Earth (usually between 30° and 60° latitude from the equator), either through cyclogenesis or extratropical transition.
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Organization of the low improved throughout the day as environmental conditions favored tropical cyclogenesis.
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However, tropical cyclogenesis is possible at any time of the year, as shown by the formation of Tropical Storm Alberto on May 25, which marked the fourth consecutive year in which a storm developed before the official start of the season.
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The Rocky Mountains block Pacific-sourced moisture and buckle the atmospheric flow, forcing drier air at mid-levels of the troposphere due to downsloping winds and causing cyclogenesis downstream to the east of the mountains.
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Centered about 100 miles (160 km) northeast of Bocas Town, Bocas del Toro, the storm remained stationary for 24 hours after tropical cyclogenesis.
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Tropical cyclogenesis is particularly common in the northern reaches of the Indian Ocean in and around the Bay of Bengal.
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The cyclogenesis of Tropical Storm Emily was complicated, extending over several days from late July into early August.
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Tropical cyclogenesis began at the end of July, with the development of Hurricane Alex on July 31.
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Cyclogenesis: the birth of a storm.
Me alegra no haberlo decepcionadoLiterature Literature
Main article: Cyclogenesis
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The Isthmus of Tehuantepec is among eight main zones of cyclogenesis worldwide.
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Elsewhere, the end of the 1990s was marked by a period of active cyclogenesis, particularly during the 1995 season.
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The main circulation alterations related to droughts describe in most cases the following: a) significant mountain range gradients, in this case we include the one that intensifies the western zonal flow (west-east) over Patagonia, which generates an anticyclogenesis on the Pacific Ocean coast and a cyclogenesis on the continent, b) anticyclonic subsidence, c) weakness of the north humid flow due to a diminution of the gradient between the Atlantic Ocean anticyclone and the continental depression and/or subsidence associated with the flow hr/>The aim of this study is to detect the possible causes of the May-to-July rainfall (MJJ) over the Limay and Neuquén river basins.
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Storm The weekend of February 8 meteorological services had predicted that a new explosive cyclogenesis, called ‘Stephanie‘, would be very close to the Cantabrian and Atlantic coasts in meteorológicos
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87 sinne gevind in 11 ms. Hulle kom uit baie bronne en word nie nagegaan nie.