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Record 1 2011-08-02

English

Subject field(s)
  • Atmospheric Physics
  • Air Pollution
DEF

A layer in the atmosphere where temperature increases with altitude instead of falling with height, and where the following characteristics can be observed: the layer is marked by its static stability and hence by the fact that very little turbulent exchanges can occur within it; strong wind shears often occur across it; abrupt changes in concentrations of atmospheric particulates and atmospheric water vapour may be encountered on ascending through it; the upward diffusion of gases is inhibited by it.

OBS

temperature inversion: this term is also used to denote the phenomenon by which that inversion layer is produced.

French

Domaine(s)
  • Physique de l'atmosphère
  • Pollution de l'air
CONT

Dans les conditions normales, la température de l'air décroît avec l'altitude; mais, si une masse d'air froid se forme au voisinage du sol (pendant les matinées d'hiver ensoleillées, et surtout dans les vallées), il apparaît une zone d'inversion de température à 200 m du sol. Les fumées et gaz polluants ne peuvent plus s'élever dans l'air et la pollution atmosphérique de la ville peut atteindre le seuil d'alerte.

Spanish

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