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Fiche 1,  Justifications,  Anglais

Record number: 1, Textual support number: 1 CONT

Generally(apart from small-scale and convective processes and flows over steep topography), the vertical wind component is much smaller than the horizontal wind components.  2, fiche 1, Anglais, - horizontal%20wind%20component

Fiche 1,  Justifications,  Français

Fiche 1,  Justifications,  Espagnol

Fiche 2,  Justifications,  Anglais

Record number: 2, Textual support number: 1 CONT

Generally(apart from small-scale and convective processes and flows over steep topography), the vertical wind component is much smaller than the horizontal wind components.  2, fiche 2, Anglais, - vertical%20wind%20component

Fiche 2,  Justifications,  Français

Fiche 2,  Justifications,  Espagnol

Fiche 3,  Justifications,  Anglais

Record number: 3, Textual support number: 1 CONT

As the wind or water current [changes] direction, your boat will swing about its anchor. This is a swing circle centred around the position of the anchor, with a radius equal to the boat's length plus the horizontal component of the length of the anchor line in use...  1, fiche 3, Anglais, - swing%20about%20its%20anchor

Fiche 3,  Justifications,  Français

Record number: 3, Textual support number: 1 DEF

Changer de direction, cap pour cap, en parlant d'un navire qui tourne autour de son ancre sous l'effet du vent ou de la marée, ou que l'on fait tourner sur place au moyen de remorqueurs ou d'amarres.  2, fiche 3, Français, - %C3%A9viter%20sur%20son%20ancre

Fiche 3,  Justifications,  Espagnol

Fiche 4,  Justifications,  Anglais

Record number: 4, Textual support number: 1 CONT

If the strong horizontal temperature gradient associated with a front maintains a near constant direction through a deep layer of the atmosphere, the thermal wind component will have a constant direction through successively higher layers. As this component is added consecutively to the actual wind at each level, the wind will increase markedly with height. This is how the very strong winds of frontal jet streams originate.  1, fiche 4, Anglais, - frontal%20jet%20stream

Fiche 4,  Justifications,  Français

Record number: 4, Textual support number: 1 CONT

Si le fort gradient de température horizontal associé à un front conserve une direction presque constante à travers une couche profonde de l’atmosphère, le vent thermique a une direction constante dans des couches de plus en plus élevées. À mesure que cette composante s’ajoute consécutivement aux vents réels à chaque niveau, le vent augmente nettement avec l’altitude. C’est ainsi que naissent les très forts vents des courants-jets frontaux.  1, fiche 4, Français, - courant%2Djet%20frontal

Fiche 4,  Justifications,  Espagnol

Fiche 5,  Justifications,  Anglais

Record number: 5, Textual support number: 1 DEF

Component of the wind in the direction opposite to that of the horizontal pressure gradient.  2, fiche 5, Anglais, - countergradient%20wind

Fiche 5,  Justifications,  Français

Record number: 5, Textual support number: 1 DEF

Composante du vent dans la direction opposée de celle du gradient horizontal de pression.  2, fiche 5, Français, - vent%20contre%20le%20gradient

Fiche 5,  Justifications,  Espagnol

Record number: 5, Textual support number: 1 DEF

Componente del viento en dirección opuesta a la del gradiente horizontal de la presión.  1, fiche 5, Espagnol, - viento%20contragradiente

Fiche 6,  Justifications,  Anglais

Record number: 6, Textual support number: 1 DEF

Theoretical wind which results from the equilibrium between the horizontal pressure force and the horizontal component of the deviating force due to the Earth's rotation, only these forces being supposed to act on the air.  2, fiche 6, Anglais, - geostrophic%20wind

Record number: 6, Textual support number: 1 OBS

It blows parallel to straight isobars or contours.  2, fiche 6, Anglais, - geostrophic%20wind

Fiche 6,  Justifications,  Français

Record number: 6, Textual support number: 1 DEF

Vent théorique résultant de l'équilibre entre la force horizontale de pression et la force déviante horizontale, supposées agir seules sur l'air.  2, fiche 6, Français, - vent%20g%C3%A9ostrophique

Record number: 6, Textual support number: 1 OBS

Il souffle parallèlement aux isobares ou isohypses rectilignes.  2, fiche 6, Français, - vent%20g%C3%A9ostrophique

Fiche 6,  Justifications,  Espagnol

Record number: 6, Textual support number: 1 DEF

Viento teórico que resulta del equilibrio entre la fuerza horizontal de presión y la componente horizontal de la fuerza desviadora debida a la rotación de la Tierra, en la hipótesis de que son las únicas fuerzas que actúan sobre el aire.  1, fiche 6, Espagnol, - viento%20geostr%C3%B3fico

Record number: 6, Textual support number: 1 OBS

Sopla paralelamente a las isobaras o isohipsas rectas.  1, fiche 6, Espagnol, - viento%20geostr%C3%B3fico

Fiche 7,  Justifications,  Anglais

Record number: 7, Textual support number: 1 CONT

The geostrophic wind approximations are broken into its two horizontal components. The "U" component represents the east-west component of the wind while the "V" component represents the north-south component. The two formulas for the U and V component of wind are as follows... The minus sign in front of the U component answer indicates an easterly component to the wind, or in other words, a wind that blows from east to west. A positive U component would mean that the wind is blowing from west to east.  1, fiche 7, Anglais, - U%20component%20of%20wind

Fiche 7,  Justifications,  Français

Record number: 7, Textual support number: 1 CONT

Composante U (méridienne) du vent à 10 mètres (positive à l'est). Unité : m/s^-1.  1, fiche 7, Français, - composante%20U%20du%20vent

Fiche 7,  Justifications,  Espagnol

Fiche 8,  Justifications,  Anglais

Record number: 8, Textual support number: 1 CONT

The geostrophic wind approximations are broken into its two horizontal components. The "U" component represents the east-west component of the wind while the "V" component represents the north-south component. The two formulas for the U and V component of wind are as follows... The positive V component answer indicates a southerly component to the wind, or in other words, a wind that blows from south to north. A negative V component would mean that the wind is blowing from north to south.  1, fiche 8, Anglais, - V%20component%20of%20wind

Fiche 8,  Justifications,  Français

Record number: 8, Textual support number: 1 CONT

Composante V (zonale) du vent à 10 mètres (positive au nord). Unité : m/s^-1.  1, fiche 8, Français, - composante%20V%20du%20vent

Fiche 8,  Justifications,  Espagnol

Fiche 9,  Justifications,  Anglais

Record number: 9, Textual support number: 1 DEF

The rainfall which is deflected, by strong winds, from its normal vertical fall and is intercepted by the walls of buildings.  2, fiche 9, Anglais, - driving%20rain%20on%20buildings

Record number: 9, Textual support number: 1 CONT

Numerical calculation of driving rain on buildings. Rain, which is given a horizontal velocity component by the influence of wind, is termed wind-driven or driving rain. Driving rain is one of the main sources to the amount of moisture a building is exposed to, and thereby contributes to the processes deteriorating the building envelope. Knowledge about the exposure of a building to driving rain is needed in order to minimise the deteriorating processes, and thus contributes to ensure a satisfactory performance of the building design.  3, fiche 9, Anglais, - driving%20rain%20on%20buildings

Fiche 9,  Justifications,  Français

Record number: 9, Textual support number: 1 DEF

Pluie qui est défléchie, par de forts vents, de sa trajectoire verticale normale et interceptée par les murs des bâtiments.  1, fiche 9, Français, - pluie%20chass%C3%A9e%20sur%20les%20b%C3%A2timents

Fiche 9,  Justifications,  Espagnol

Record number: 9, Textual support number: 1 DEF

Lluvia que durante períodos de vientos fuertes es desviada de la vertical por el viento y es interceptada por los edificios.  1, fiche 9, Espagnol, - lluvia%20impulsada%20por%20el%20viento%20contra%20los%20edificios

Fiche 10,  Justifications,  Anglais

Record number: 10, Textual support number: 1 CONT

Driving rain is rain that is carried by the wind and driven onto the building envelope (façades and roofs). It is a complex phenomenon of falling raindrops in a turbulent flow of wind around a building. It is one of the important climatological factors which determine long-term use and durability of building envelopes.  6, fiche 10, Anglais, - driving%20rain

Record number: 10, Textual support number: 2 CONT

Numerical calculation of driving rain on buildings. Rain, which is given a horizontal velocity component by the influence of wind, is termed wind-driven or driving rain. Driving rain is one of the main sources to the amount of moisture a building is exposed to, and thereby contributes to the processes deteriorating the building envelope. Knowledge about the exposure of a building to driving rain is needed in order to minimise the deteriorating processes, and thus contributes to ensure a satisfactory performance of the building design.  7, fiche 10, Anglais, - driving%20rain

Fiche 10,  Justifications,  Français

Record number: 10, Textual support number: 1 CONT

La pénétration de la pluie qui est causée par les pressions du vent constitue un problème important du point de vue de la performance en construction, mais au fur et à mesure que l'on en connaîtra davantage sur le rapport entre la pluie et le vent, il sera possible de concevoir de façon économique des édifices qui sont plus en mesure de résister à la pluie chassée par le vent.  2, fiche 10, Français, - pluie%20chass%C3%A9e%20par%20le%20vent

Record number: 10, Textual support number: 2 CONT

Exposition à de la pluie chassée par le vent en provenance de toutes les directions.  3, fiche 10, Français, - pluie%20chass%C3%A9e%20par%20le%20vent

Fiche 10,  Justifications,  Espagnol

Fiche 11,  Justifications,  Anglais

Record number: 11, Textual support number: 1 DEF

Line along which there is an abrupt change in the horizontal wind component parallel to this line.  2, fiche 11, Anglais, - shear%20line

Fiche 11,  Justifications,  Français

Record number: 11, Textual support number: 1 DEF

Ligne le long de laquelle il y a une variation abrupte de la composante horizontale du vent parallèle à cette ligne.  2, fiche 11, Français, - ligne%20de%20cisaillement

Fiche 11,  Justifications,  Espagnol

Record number: 11, Textual support number: 1 DEF

Línea a lo largo de la cual hay un cambio brusco en la componente horizontal del viento paralelo a dicha línea.  1, fiche 11, Espagnol, - l%C3%ADnea%20de%20cortante

Fiche 12,  Justifications,  Anglais

Record number: 12, Textual support number: 1 DEF

Theoretical wind which ... blows parallel to curved isobars or contours.  2, fiche 12, Anglais, - gradient%20wind

Record number: 12, Textual support number: 1 OBS

... wind resulting from the equilibrium between the horizontal pressure force, the horizontal component of the deviating force due to the Earth's rotation, and the centrifugal force due to air motion on a curved path, only these forces being supposed to act on the air.  2, fiche 12, Anglais, - gradient%20wind

Record number: 12, Textual support number: 2 OBS

gradient wind: term officially approved by the International Civil Aviation Organization (ICAO).  3, fiche 12, Anglais, - gradient%20wind

Fiche 12,  Justifications,  Français

Record number: 12, Textual support number: 1 DEF

Vent théorique [qui] souffle parallèlement aux isobares ou aux isohypses.  3, fiche 12, Français, - vent%20du%20gradient

Record number: 12, Textual support number: 1 OBS

Vent théorique résultant de l'équilibre entre la force horizontale de pression, la force déviante horizontale et la force centrifuge due à la courbure de la trajectoire de l'air, supposées agir seules sur l'air.  4, fiche 12, Français, - vent%20du%20gradient

Record number: 12, Textual support number: 2 OBS

vent du gradient : terme uniformisé par l'Organisation de l'aviation civile internationale (OACI).  5, fiche 12, Français, - vent%20du%20gradient

Fiche 12,  Justifications,  Espagnol

Record number: 12, Textual support number: 1 DEF

Viento teórico [que] sopla paralelamente a las isobaras o isohipsas curvas.  2, fiche 12, Espagnol, - viento%20del%20gradiente

Record number: 12, Textual support number: 1 OBS

Viento teórico resultante del equilibrio entre la fuerza horizontal de presión, la componente horizontal de la fuerza desviadora debida a la rotación de la Tierra y la fuerza centrífuga debida al movimiento del aire en una trayectoria curva, en la hipótesis de que son las únicas fuerzas que actúan sobre el aire.  2, fiche 12, Espagnol, - viento%20del%20gradiente

Record number: 12, Textual support number: 2 OBS

viento del gradiente : término aceptado oficialmente por la Organización de Aviación Civil Internacional (OACI).  3, fiche 12, Espagnol, - viento%20del%20gradiente

Fiche 13,  Justifications,  Anglais

Record number: 13, Textual support number: 1 CONT

In the cylindrical coordinate representation, most commonly used for reporting wind measurements, the horizontal wind is represented by a 2-D vector magnitude speed, and a direction [theta](the same as in the spherical representation), plus the vertical component(positive upward as in the cartesian representation).  1, fiche 13, Anglais, - cylindrical%20coordinate%20representation

Fiche 13,  Justifications,  Français

Fiche 13,  Justifications,  Espagnol