le sens du vent – English Translation – Keybot Dictionary

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  catalogo.stilolinea.it  
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Prenez un équipier à bord, il vous montrera la boussole pendant que vous tiendrez la barre. Nos coaches n'ont pas leurs pareils pour vous aider à développer vos propres ressources et vous faire sentir le sens du vent.
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Travelling solely in the desired direction is not always plain sailing. If you take a sailor on board, he could hold the compass while you steer the ship! If you want an individual approach, custom made for your personal needs, then this is the vessel you should board. By doing this you can find answers from your own capabilities and competences , and feel which way the wind is blowing.
  www.westcottbrand.ca  
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Le sens du vent
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Conversations
  www.hc-sc.gc.ca  
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La dérive de pulvérisation se produit lors de l'application d'un pesticide si les gouttelettes émises par l'équipement de pulvérisation sont transportées dans le sens du vent (vent arrière) en dehors de la zone ciblée par le traitement au site d'application.
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Vapour drift occurs if a pesticide evaporates from the sprayed material during application or from surfaces such as soil or plants after application. The volatilized pesticide can then be transported by the wind.
  hc-sc.gc.ca  
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La dérive de pulvérisation se produit lors de l'application d'un pesticide si les gouttelettes émises par l'équipement de pulvérisation sont transportées dans le sens du vent (vent arrière) en dehors de la zone ciblée par le traitement au site d'application.
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Vapour drift occurs if a pesticide evaporates from the sprayed material during application or from surfaces such as soil or plants after application. The volatilized pesticide can then be transported by the wind.
  blog.crowdestate.eu  
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Cet étage est occupé par des plantes à fleurs, adaptées à ces contraintes. La présence de vent, généralement important sur le littoral, peut façonner la tenue de la végétation, orientée alors dans le sens du vent,
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The halophile stage, which is composed entirely of mainland, but which is influenced by the sprays composed of currents of air charged with droplets of salt water, which therefore carry “salts” and “humidity”. This stage is occupied by flowering plants that are adapted to these conditions. The presence of the wind, which is generally important on the coastline, can shape the vegetation’s hold, as it leans according to the direction of the wind,
  www.tides.gc.ca  
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Le vent et les différences de pression barométrique à la surface d'un lac peuvent en effet créer des écarts de niveau d'eau temporaires en différents endroits. Les ondes de tempête sont particulièrement fortes aux extrémités d'un bassin allongé, surtout lorsque l'axe longitudinal du bassin est dans le sens du vent.
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These fluctuations, lasting from a less than an hour to several days, are caused by meteorological conditions. The effect of wind and differences in barometric pressure over the lake surface create temporary imbalances in the water level at various locations. Storm surges are largest at the ends of an elongated basin, particularly when the long axis of the basin is aligned with the wind. In deep lakes such as Lake Ontario, the surge of water level rarely exceeds 0.5 metre, but in shallow Lake Erie, water-level differences from one end of the lake to the other of more than 5 metres have been observed. Although the range of fluctuations may be large, there are only minor changes in the volume of water in the lake. A seiche is the free oscillation of water in a closed or semi-closed basin; it is frequently observed in harbours, bays, lakes and in almost any distinct basin of moderate size.
  tides.gc.ca  
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Le vent et les différences de pression barométrique à la surface d'un lac peuvent en effet créer des écarts de niveau d'eau temporaires en différents endroits. Les ondes de tempête sont particulièrement fortes aux extrémités d'un bassin allongé, surtout lorsque l'axe longitudinal du bassin est dans le sens du vent.
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These fluctuations, lasting from a less than an hour to several days, are caused by meteorological conditions. The effect of wind and differences in barometric pressure over the lake surface create temporary imbalances in the water level at various locations. Storm surges are largest at the ends of an elongated basin, particularly when the long axis of the basin is aligned with the wind. In deep lakes such as Lake Ontario, the surge of water level rarely exceeds 0.5 metre, but in shallow Lake Erie, water-level differences from one end of the lake to the other of more than 5 metres have been observed. Although the range of fluctuations may be large, there are only minor changes in the volume of water in the lake. A seiche is the free oscillation of water in a closed or semi-closed basin; it is frequently observed in harbours, bays, lakes and in almost any distinct basin of moderate size.
  www.marees.gc.ca  
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Le vent et les différences de pression barométrique à la surface d'un lac peuvent en effet créer des écarts de niveau d'eau temporaires en différents endroits. Les ondes de tempête sont particulièrement fortes aux extrémités d'un bassin allongé, surtout lorsque l'axe longitudinal du bassin est dans le sens du vent.
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TThese fluctuations, lasting from a less than an hour to several days, are caused by meteorological conditions. The effect of wind and differences in barometric pressure over the lake surface create temporary imbalances in the water level at various locations. Storm surges are largest at the ends of an elongated basin, particularly when the long axis of the basin is aligned with the wind. In deep lakes such as Lake Ontario, the surge of water level rarely exceeds 0.5 metre, but in shallow Lake Erie, water-level differences from one end of the lake to the other of more than 5 metres have been observed. Although the range of fluctuations may be large, there are only minor changes in the volume of water in the lake. A seiche is the free oscillation of water in a closed or semi-closed basin; it is frequently observed in harbours, bays, lakes and in almost any distinct basin of moderate size.
  tides-marees.gc.ca  
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Le vent et les différences de pression barométrique à la surface d'un lac peuvent en effet créer des écarts de niveau d'eau temporaires en différents endroits. Les ondes de tempête sont particulièrement fortes aux extrémités d'un bassin allongé, surtout lorsque l'axe longitudinal du bassin est dans le sens du vent.
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TThese fluctuations, lasting from a less than an hour to several days, are caused by meteorological conditions. The effect of wind and differences in barometric pressure over the lake surface create temporary imbalances in the water level at various locations. Storm surges are largest at the ends of an elongated basin, particularly when the long axis of the basin is aligned with the wind. In deep lakes such as Lake Ontario, the surge of water level rarely exceeds 0.5 metre, but in shallow Lake Erie, water-level differences from one end of the lake to the other of more than 5 metres have been observed. Although the range of fluctuations may be large, there are only minor changes in the volume of water in the lake. A seiche is the free oscillation of water in a closed or semi-closed basin; it is frequently observed in harbours, bays, lakes and in almost any distinct basin of moderate size.