Concerning the origin of enhanced sodium layers

Details Concerning the origin of enhanced sodium layers Concerning the origin of enhanced sodium layers

Oct 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988georl..15.1267c&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 15, Oct. 1988, p. 1267-1270.

Physics

29

Atmospheric Composition, Sodium, Wind Shear, Gravity Waves, Vertical Distribution, Wind Effects

Scientific paper

A mechanism is proposed for the formation of the thin layers of enhanced concentration observed in the atmospheric layer. The proposed mechanism involves the wind-shear distortion of initially thick Na clouds of limited horizontal extent, originally produced by the deposition of material of extraterrestrial origin. This mechanism explains almost all the observed characteristics of the enhanced layers, including their height of occurrence, small vertical extent, vertical motion, rapid growth and decay, and highly variable duration.

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