Show simple item record

dc.contributor.authorMange, P.
dc.coverage.temporal20th century
dc.date1957
dc.date.accessioned2016-03-07T17:14:01Z
dc.date.accessioned2021-12-09T09:52:32Z
dc.date.available2016-03-07T17:14:01Z
dc.date.available2021-12-09T09:52:32Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8311
dc.descriptionThe mathematical theory of minor-constituent neutral-particle diffusion is reviewed and extended to take account of diffusion in an atmosphere with linearly varying scale height. In addition, solutions of sinks and sources (simultaneous production). Various simplified criteria of diffusion which have been used formerly are reviewed, and a general criterion is proposed. Application of the general theory to three particular problems is briefly indicated. In the first, it is shown that under the simultaneous action of diffusion and mixing the molecular oxygen distribution above 100-km altitude must depart from a photochemical equilibrium distribution. Secondly, the downward migration of calcium continuously introduced into the atmosphere by meteor is described ; and, finally, the usefulness is the theory is shown in analyzing the downward migration of nitrogen atoms from a high-level production regions.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesContributions, n° - Bijdragen, nr.
dc.titleThe theory of molecular diffusion in the atmosphere
dc.typeBook
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeMolecular diffusion
dc.subject.freeAtmosphere
dc.source.volume35
dc.source.page18
Orfeo.peerreviewedYes


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record