Logo
Unionpedia
Communication
Get it on Google Play
New! Download Unionpedia on your Android™ device!
Free
Faster access than browser!
 

Brewer–Dobson circulation and G. M. B. Dobson

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Brewer–Dobson circulation and G. M. B. Dobson

Brewer–Dobson circulation vs. G. M. B. Dobson

Brewer–Dobson circulation is a model of atmospheric circulation, proposed by Alan Brewer in 1949 and Gordon Dobson in 1956, which attempts to explain why tropical air has less ozone than polar air, even though the tropical stratosphere is where most atmospheric ozone is produced. Gordon Miller Bourne Dobson FRS (25 February 1889 – 11 March 1975) was a British physicist and meteorologist who did important work on ozone.

Similarities between Brewer–Dobson circulation and G. M. B. Dobson

Brewer–Dobson circulation and G. M. B. Dobson have 3 things in common (in Unionpedia): Dobson unit, Ozone, Stratosphere.

Dobson unit

The Dobson unit (DU) is a unit of measurement of the amount of a trace gas in a vertical column through the Earth's atmosphere.

Brewer–Dobson circulation and Dobson unit · Dobson unit and G. M. B. Dobson · See more »

Ozone

Ozone, or trioxygen, is an inorganic molecule with the chemical formula.

Brewer–Dobson circulation and Ozone · G. M. B. Dobson and Ozone · See more »

Stratosphere

The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere.

Brewer–Dobson circulation and Stratosphere · G. M. B. Dobson and Stratosphere · See more »

The list above answers the following questions

Brewer–Dobson circulation and G. M. B. Dobson Comparison

Brewer–Dobson circulation has 10 relations, while G. M. B. Dobson has 22. As they have in common 3, the Jaccard index is 9.38% = 3 / (10 + 22).

References

This article shows the relationship between Brewer–Dobson circulation and G. M. B. Dobson. To access each article from which the information was extracted, please visit:

Hey! We are on Facebook now! »