TERMIUM Plus®

The Government of Canada’s terminology and linguistic data bank.

AEROSOL LAYER [2 records]

Record 1 2003-11-26

English

Subject field(s)
  • Arithmetic and Number Theory
  • Climatology
DEF

A maximum in large particle concentrations observed in the lower stratosphere between 15 and 25 km.

CONT

While searching for debris from nuclear bomb tests, Christian Junge discovered in 1960 a layer of microscopic aerosol particles between the tropopause and about 18 miles (30 km) altitude. These particles are composed of sulfuric acid and water and are formed by the chemical transformation of sulfur-containing gases. This layer is called the Junge Layer or the Stratospheric Aerosol Layer.

CONT

The relative maximum of the global vertical aerosol concentration profile in the lower stratosphere is commonly referred to as the Junge aerosol layer, or simply the Junge layer. It is of great importance to study the formation of this layer and to monitor its changes because of the possible impacts of these stratospheric aerosols to global climate. At present, the formation mechanism of the Junge layer is not well understood. Current theories of Junge layer formation include the injection of sulfate particles by volcanic eruptions, turbulent diffusion of tropospheric sulfates, natural (biogenic) emissions of carbonyl sulfide, and other processes.

OBS

Stratospheric aerosols have a maximum concentration around 20 km and contain large fractions of sulfate.

OBS

It is a worldwide phenomenon.

Key term(s)
  • stratospheric Junge layer

French

Domaine(s)
  • Arithmétique et théorie des nombres
  • Climatologie
DEF

Couche d'aérosols de plusieurs kilomètres d'épaisseur située dans la stratosphère à une altitude d'environ 20 km

CONT

Les sulfates disparaissent brusquement de la couche d'aérosols stratosphériques au-delà de 22-23 km d'altitude [...] Il semble donc qu'ils apparaîtraient à ce niveau par réaction [de l'acide sulfurique] néoformé sur l'ammoniac et qu'ils se sédimentent lentement vers le sol. Cette couche joue donc un rôle important dans le cycle biogéochimique du soufre et dans une moindre mesure dans celui de l'azote.

Key term(s)
  • couche d'aérosols de Junge

Spanish

Campo(s) temático(s)
  • Aritmética y teoría de los números
  • Climatología
DEF

Concentración máxima de partículas grandes observada en la estratosfera baja entre 15 y 25 km.

OBS

Es un fenómeno mundial.

Save record 1

Record 2 1991-05-13

English

Subject field(s)
  • Climatology
  • Pollutants
CONT

Non-absorbing aerosols increase the albedo of the atmosphere and reduce the amount of solar radiation that reaches the surface. If the aerosol absorbs in the shortwave range of the spectrum, energy is directly transferred to the atmosphere. The effect is heating of the atmosphere and cooling of the underlying surface. ... The net effect depends on the ratio of the absorption coefficients in the visible and infrared but also on the albedo of the surface and the altitude of the aerosol layer.

French

Domaine(s)
  • Climatologie
  • Agents de pollution
CONT

Si le coefficient de réflexion moyen est plus grand dans l'infra-rouge que dans le visible, les températures au sol s'élèveront. Elles décroîtront dans l'hypothèse inverse. Mais l'absorption intervient aussi dans le coefficient. En effet, les particules captent une partie de l'énergie reçue. Là encore, l'altitude de la couche d'aérosols joue un grand rôle.

Spanish

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