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Fiche 1,  Justifications,  Anglais

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Regarding the general distinction(in meteorology) between advection and convection, the former describes the predominantly horizontal, large-scale motions of the atmosphere, while convection describes the predominantly vertical, locally induced motions.  2, fiche 1, Anglais, - advection

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advection: designation standardized by ISO.  3, fiche 1, Anglais, - advection

Fiche 1,  Justifications,  Français

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[...] transport des propriétés d'une masse d'air par le champ de vitesse de l'atmosphère.  2, fiche 1, Français, - advection

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En météorologie, l'advection décrit les grands mouvements atmosphériques à prédominance horizontale, tandis que la convection est confinée aux mouvements locaux à dominance verticale.  2, fiche 1, Français, - advection

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advection : désignation normalisée par l'ISO.  3, fiche 1, Français, - advection

Fiche 1,  Justifications,  Espagnol

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Transporte de las propiedades de una masa de aire producido por el campo de velocidades de la atmósfera.  2, fiche 1, Espagnol, - advecci%C3%B3n

Fiche 2,  Justifications,  Anglais

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Meteorologists describe the horizontal movement of cold and warm air by the wind as temperature advection... Specifically, cold-air advection... describes the horizontal transport of cold air by the wind... cold-air advection causes local temperatures to decrease with time, and [it is] the primary cause of temperature decreases behind cold frontal passages.  3, fiche 2, Anglais, - cold%20air%20advection

Fiche 2,  Justifications,  Français

Fiche 2,  Justifications,  Espagnol

Fiche 3,  Justifications,  Anglais

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Basically[, ] marine fog represented by the [climate] model is warm air advection fog, and it was found that the change in the horizontal temperature advection near the surface mostly determines the changes in marine fog in a warmer climate. Therefore, the changes in marine fog can be almost explained by the large-scale circulation changes. On the other hand, in-cloud LWC(liquid water content) of the fog is consistently increased in a warmer climate for the same horizontal surface temperature advection.  2, fiche 3, Anglais, - warm%2Dair%20advection%20fog

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Fiche 3,  Justifications,  Espagnol

Fiche 4,  Justifications,  Anglais

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Meteorologists describe the horizontal movement of cold and warm air by the wind as temperature advection... Specifically,... warm-air advection... represents the horizontal transport of warm air by the wind. Acting alone, warm-air advection causes local temperatures to increase with time, and is the primary cause of temperature increases associated with warm frontal passages.  3, fiche 4, Anglais, - warm%20air%20advection

Fiche 4,  Justifications,  Français

Fiche 4,  Justifications,  Espagnol

Fiche 5,  Justifications,  Anglais

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Horizontal temperature advection plays an especially prominent role in affecting winter climate over continental interiors, where both climatological conditions and extreme weather are strongly regulated by transport of remote air masses.  1, fiche 5, Anglais, - horizontal%20temperature%20advection

Fiche 5,  Justifications,  Français

Fiche 5,  Justifications,  Espagnol

Fiche 6,  Justifications,  Anglais

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It is important to note that convective cells can cause air currents both upward and downward. Upward convective currents carry pollutants many kilometers high into the atmosphere. At these high altitudes advective currents and prevailing winds can transport these pollutants vast distances very quickly. As air spreads from the rising column, it is cooled and falls back down to the earth. This results in a circular rotation of the air.  3, fiche 6, Anglais, - advective%20current

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Drainage of the lake-beds, related to a seasonal phenomenon of dust storms between February and May, has also affected air quality. The midday air temperatures during the dry season generate strong advective currents that elevate salt and clay particles from the former lake bottom. These particles are blown into the city by the prevailing easterly winds.  1, fiche 6, Anglais, - advective%20current

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advective: of, or caused by, advection.  4, fiche 6, Anglais, - advective%20current

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advection : the transfer of heat by the horizontal movement of the air.  4, fiche 6, Anglais, - advective%20current

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advection : The horizontal movement of air around the world is known as advection. Advection is the primary mechanism responsible for long range transport of pollutants. Although transport of pollutants via advection is minuscule at the earth's surface, at heights above 1000 m, where friction become negligible, wind velocities of 400 km/hr can carry pollutants at extremely fast rates.  3, fiche 6, Anglais, - advective%20current

Fiche 6,  Justifications,  Français

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Les masses d'air polluées et riches en ozone sont d'abord transportées vers la région de l'Atlantique par la cellule de haute pression qui se dirige vers l'est. La cellule se déplace le long de la côte est de l'Amérique du Nord, créant une poussée d'air du sud ou du sud-ouest qui dirige les polluants par advection dans la région de l'Atlantique.  3, fiche 6, Français, - courant%20d%27advection

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advection : Transfert des propriétés d'une masse d'air par déplacement, notamment dans le plan horizontal.  4, fiche 6, Français, - courant%20d%27advection

Fiche 6,  Justifications,  Espagnol

Fiche 7,  Justifications,  Anglais

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A surface separating two fluids, across which there is a discontinuity of some fluid property, such as density, velocity, etc., or of some derivative of one of these properties in a direction normal to the interface.  3, fiche 7, Anglais, - internal%20boundary%20layer

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Internal boundary layers are associated with the horizontal advection of air across a discontinuity in some property of the surface(e. g., aerodynamic roughness length or surface heat flux) and can be viewed as layers in which the atmosphere is adjusting to new surface properties.  2, fiche 7, Anglais, - internal%20boundary%20layer

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... the equations of motion do not apply at the interface but are replaced by the kinematic and dynamic boundary conditions.  3, fiche 7, Anglais, - internal%20boundary%20layer

Fiche 7,  Justifications,  Français

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Surface de séparation de deux fluides caractérisée par une discontinuité d'une propriété de ces fluides, telle que densité, vitesse, etc., ou d'une dérivée quelconque d'une de ces propriétés dans une direction normale à l'interface.  1, fiche 7, Français, - couche%20limite%20interne

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Les équations du mouvement ne s'appliquent donc pas à l'interface; elles sont remplacées par les conditions aux limites cinématiques et dynamiques.  1, fiche 7, Français, - couche%20limite%20interne

Fiche 7,  Justifications,  Espagnol

Record number: 7, Textual support number: 1 DEF

Superficie de separación entre dos fluidos en la que hay una discontinuidad de alguna propiedad del fluido, como la densidad, la velocidad, etc., o de algún derivado de una de esas propiedades en una dirección normal al interfaz.  1, fiche 7, Espagnol, - capa%20l%C3%ADmite%20interna

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Por consiguiente, las ecuaciones de movimiento no se aplican al interfaz, sino que son sustituidas por las condiciones límites cinemáticas y dinámicas.  1, fiche 7, Espagnol, - capa%20l%C3%ADmite%20interna