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Record 1,  Textual support,  English

Record number: 1, Textual support number: 1 CONT

Raised peatland swamps occur as raised plateaus, similar to and often transitional to domed bogs, but there is minerotrophic groundwater influence. These are similar to mineral-rise swamps but are elevated by peat and are situated entirely in peatland terrain.  1, record 1, English, - raised%20peatland%20swamp

Record 1,  Textual support,  French

Record number: 1, Textual support number: 1 CONT

Les marécages de tourbière élevée se trouvent sur des plateaux élevés, semblables aux bogs bombés ou souvent en transition pour le devenir, mais sans l'effet de l'eau souterraine minérotrophe. Ils sont semblables aux marécages de butte minérale, mais sont élevés en raison de la tourbe et situés entièrement dans les tourbières.  1, record 1, French, - mar%C3%A9cage%20de%20tourbi%C3%A8re%20%C3%A9lev%C3%A9e

Record 1,  Textual support,  Spanish

Record 2,  Textual support,  English

Record number: 2, Textual support number: 1 CONT

Surface Roughness. The surface of the ground has a major influence on early season avalanching. Roughness of surface determines the snow depth needed to fill irregularities, controls the amount of creep and significantly affects the ability of the snow to avalanche to the ground in many regions. Generally, the rougher the ground surface the more snow depth is required before avalanching will take place; broken terrain and boulder fields won’t become avalanche slopes until sufficient snow has fallen to cover most of the rocks.... Professional hazard evaluators are using a figure of 30 to 60 cm, depending on location, as the minimum snow depth necessary to cover roughness of ground before natural avalanching occurs. This figure applies to many areas but should not be taken as an infallible rule of thumb.  2, record 2, English, - ground%20roughness

Record number: 2, Textual support number: 2 CONT

A 1-metre snowpack will typically cover all of the ground roughness. [Example approved by the Avalanche Bulletin Terminology Standardization Committee.]  1, record 2, English, - ground%20roughness

Record number: 2, Textual support number: 1 OBS

Rough ground will anchor the snowpack until it is deep enough to form a relatively smooth surface. Bedrock, boulders (about 2 or 3 m apart), stumps, logs, short stiff shrubs, and benches are all surface features that provide good anchors to hold the snowpack.  4, record 2, English, - ground%20roughness

Record number: 2, Textual support number: 2 OBS

ground roughness: term officially approved by the Avalanche Bulletin Terminology Standardization Committee.  5, record 2, English, - ground%20roughness

Record 2,  Textual support,  French

Record number: 2, Textual support number: 1 CONT

Un manteau neigeux d'une épaisseur de 1 m est généralement suffisant pour recouvrir la rugosité du sol. [Exemple entériné par le Comité d'uniformisation de la terminologie des bulletins d'avalanche.]  2, record 2, French, - rugosit%C3%A9%20du%20sol

Record number: 2, Textual support number: 1 OBS

rugosité du sol : terme uniformisé par le Comité d'uniformisation de la terminologie des bulletins d'avalanche.  3, record 2, French, - rugosit%C3%A9%20du%20sol

Record 2,  Textual support,  Spanish

Record 3,  Textual support,  English

Record number: 3, Textual support number: 1 DEF

Description of the geometric orientation in the horizontal plane of an object in the scene with respect to the illuminating wavefront.  2, record 3, English, - aspect%20angle

Record number: 3, Textual support number: 1 CONT

The aspect angle... can have a significant influence on the appearance of radar imagery, especially when features in the scene have an organized linear structure, such as agricultural crops or geological structures. When a radar's illumination is oriented perpendicular to geologic features such as faults, lineaments and outcrops, [there is] increased contrast and shadowing of the features in the image results. This is a favourable aspect angle for the image interpreter, as terrain is enhanced. In agricultural applications, fields imaged from different aspect angles may result in different tones on the image because of row or planting direction. Aspect angle can cause imaging geometry to be either enhanced or suppressed.  3, record 3, English, - aspect%20angle

Record number: 3, Textual support number: 1 OBS

aspect angle: term officially approved by the RADARSAT-2 Terminology Approval Group (RTAG).  4, record 3, English, - aspect%20angle

Record 3,  Textual support,  French

Record number: 3, Textual support number: 1 DEF

Description de l'orientation géométrique de l'objet ciblé dans le plan horizontal par rapport à l'éclairement lumineux du front d'onde.  2, record 3, French, - angle%20d%27aspect

Record number: 3, Textual support number: 1 OBS

angle d'aspect : terme uniformisé par le Groupe de travail de la terminologie de RADARSAT-2 (GTTR).  2, record 3, French, - angle%20d%27aspect

Record 3,  Textual support,  Spanish

Record 4,  Textual support,  English

Record number: 4, 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, record 4, English, - turbulent%20exchange%20coefficient

Record number: 4, 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, record 4, English, - turbulent%20exchange%20coefficient

Record number: 4, 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, record 4, English, - turbulent%20exchange%20coefficient

Record number: 4, Textual support number: 1 OBS

Turbulent exchange (convection) is the main process that transfers latent and sensible heat from earth to atmosphere.  7, record 4, English, - turbulent%20exchange%20coefficient

Record number: 4, Textual support number: 1 PHR

Turbulent exchange coefficient for heat, latent heat, momentum, moisture, temperature, vapor.  8, record 4, English, - turbulent%20exchange%20coefficient

Record number: 4, Textual support number: 2 PHR

Turbulent transfer coefficient of heat, water vapor, momentum.  8, record 4, English, - turbulent%20exchange%20coefficient

Record 4,  Textual support,  French

Record number: 4, 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, record 4, French, - coefficient%20d%27%C3%A9change%20turbulent

Record number: 4, 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, record 4, French, - coefficient%20d%27%C3%A9change%20turbulent

Record number: 4, Textual support number: 1 PHR

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

Record 4,  Textual support,  Spanish

Record 5,  Textual support,  English

Record number: 5, Textual support number: 1 CONT

Terrain can influence the transport and diffusion of hazardous gases to a critical degree.... Channelling of winds along valleys can lead to transport of gases with restricted lateral diffusion for considerable distances.  3, record 5, English, - horizontal%20diffusion

Record number: 5, Textual support number: 1 OBS

horizontal: parallel to the plane of the horizon; not vertical.  4, record 5, English, - horizontal%20diffusion

Record number: 5, Textual support number: 2 OBS

diffusion: The permeation of one substance through another, such as gas through gas, liquid, or solid; solute through solvent; liquid through liquid or solid; sand finally solid through solid.  5, record 5, English, - horizontal%20diffusion

Record 5,  Textual support,  French

Record number: 5, Textual support number: 1 CONT

Une cheminée est une source ponctuelle de gaz émis de façon continue [...] A) Formule de Bosanquet-Pearson. Dans le cas d'une source ponctuelle de débit constant, [...] l'équation de diffusion s'écrit : [...]. Bosanquet et Pearson intègrent cette équation en considérant successivement l'effet de la diffusion verticale et de la diffusion horizontale [...].  3, record 5, French, - diffusion%20horizontale

Record number: 5, Textual support number: 1 OBS

[...] une diffusion entre des corps possédant à peu près la même stabilité et, pratiquement, dans une même zone horizontale [...]  3, record 5, French, - diffusion%20horizontale

Record 5,  Textual support,  Spanish

Record 6,  Textual support,  English

Record number: 6, Textual support number: 1 CONT

Terrain can influence the transport and diffusion of hazardous gases to a critical degree, especially for heavier-than-air gases(such as chlorine). Channelling of winds along valleys can lead to transport of gases with restricted lateral diffusion for considerable distances. In light winds, the slope of terrain has a significant influence on local airflow.  2, record 6, English, - airflow

Record 6,  Textual support,  French

Record number: 6, Textual support number: 1 CONT

[Influence de la topographie sur le gradient de température et sur les vents]. Le relief en général exerce une action dynamique sur l'écoulement de l'air. [...] D'une façon générale, les filets d'air ont tendance à épouser plus ou moins le profil du relief, de sorte qu'une montagne engendre une zone d'ascendance de l'air sur sa face au vent suivie d'une zone de descendance.  2, record 6, French, - %C3%A9coulement%20de%20l%27air

Record 6,  Textual support,  Spanish

Record 7,  Textual support,  English

Record number: 7, Textual support number: 1 CONT

Terrain can influence the transport and diffusion of hazardous gases to a critical degree, especially for heavier-than-air gases. Channelling of winds along valleys can lead to transport of gases with restricted lateral diffusion for considerable distances. In light winds, the slope of terrain has a significant influence on local airflow. Cooled topographic features in the case of release of cold gas have resulted in slope flows....  1, record 7, English, - slope%20flow

Record 7,  Textual support,  French

Record number: 7, Textual support number: 1 OBS

Fig. 2.12. - Schéma de distribution des températures dans une vallée, mettant en évidence l'écoulement et la stagnation de l'air froid.  2, record 7, French, - %C3%A9coulement%20de%20pente

Record number: 7, Textual support number: 2 OBS

L'action thermique du relief crée un régime de vent particulier à la vallée : brises de pente, brises de vallée. La brise de pente est due à la différence de température entre le sol incliné d'un relief quelconque et l'air libre au même niveau. Sous l'influence du rayonnement solaire, le sol se réchauffe plus vite que l'air libre durant le jour. L'air, qui se trouve directement au contact du sol, tend donc à s'élever le long de la pente tandis que l'air libre s'affaisse : c'est la brise montante. La nuit au contraire, le sol refroidit par rayonnement l'air qui se trouve en contact avec lui. Cet air devenu plus lourd s'écoule le long de la pente : c'est la brise descendante. La brise de pente sera d'autant plus accentuée que la vallée sera large et que la pente sera exposée au soleil.  2, record 7, French, - %C3%A9coulement%20de%20pente

Record 7,  Textual support,  Spanish

Record 8,  Textual support,  English

Record number: 8, Textual support number: 1 CONT

Terrain influence is also discussed and the results of other workers in this field are referenced.  1, record 8, English, - terrain%20influence

Record 8,  Textual support,  French

Record 8,  Textual support,  Spanish