TERMIUM Plus^®

Fiche 1,  Justifications,  Anglais

Record number: 1, Textual support number: 1 CONT

This equation ... assumes that the major part of the turbulent transport is dominated by eddies smaller than the distance over which the gradient is measured. This requirement is not met with elevated measurement heights in a strongly convective boundary layer. Since the turbulent exchange coefficient is a property of the flow and not of the compound transported, a similarity between exchange coefficients for passive scalar properties can be assumed.  5, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Record number: 1, Textual support number: 2 CONT

The measurements over highly complex terrain document the mechanical and thermal (by differential insolation) influence of the orography on the vertical turbulent exchange. A first step towards a parameterization of the turbulent exchange coefficient over orography is proposed.  6, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Record number: 1, Textual support number: 3 CONT

By analogy with molecular diffusion, the eddy flux in the planetary boundary layer is often expressed by ... where K_sigma is the turbulent transfer coefficient (also turbulent exchange coefficient, or eddy diffusivity).  2, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Record number: 1, Textual support number: 1 OBS

Turbulent exchange (convection) is the main process that transfers latent and sensible heat from earth to atmosphere.  7, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Record number: 1, Textual support number: 1 PHR

Turbulent exchange coefficient for heat, latent heat, momentum, moisture, temperature, vapor.  8, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Record number: 1, Textual support number: 2 PHR

Turbulent transfer coefficient of heat, water vapor, momentum.  8, fiche 1, Anglais, - turbulent%20exchange%20coefficient

Fiche 1,  Justifications,  Français

Record number: 1, Textual support number: 1 CONT

Le transport vertical des gaz CO₂ et CH₄ sous forme dissoute dans le réservoir se fait par diffusion turbulente et par mélange convectif. Deux formulations du paramétrage du transfert des gaz vers l'atmosphère ont été testées pour l'estimation des flux de GES [gaz à effet de serre] à la surface des réservoirs. La première formulation fait appel aux coefficients d'échanges turbulents alors que la seconde s'apparente à un modèle de couche-limite.  2, fiche 1, Français, - coefficient%20d%27%C3%A9change%20turbulent

Record number: 1, Textual support number: 2 CONT

Le coefficient h_s dépend du coefficient d'échange turbulent h_a, de la conductance de surface du sol et des conductances stomatiques des différentes feuilles du couvert végétal.  3, fiche 1, Français, - coefficient%20d%27%C3%A9change%20turbulent

Record number: 1, Textual support number: 1 PHR

Coefficient d'échange turbulent de chaleur, de quantité de mouvement, d'humidité.  4, fiche 1, Français, - coefficient%20d%27%C3%A9change%20turbulent

Fiche 1,  Justifications,  Espagnol