The terrestrial potassium layer (75-110 km) between 71°S and 54°N: Observations and modeling

• Published in: Journal of Geophysical Research: Space Physics 1999-08, Vol.104 (A8), p.17173-17186
• Main Authors: Eska, V., Zahn, U., Plane, J. M. C.
• Format: Article
• Language: English
• Subjects: Cosmic dust; Earth, ocean, space; Exact sciences and technology; External geophysics; Physics of the high neutral atmosphere
• ISSN: 0148-0227; 2156-2202
• DOI: 10.1029/1999JA900117

Observations of the nighttime atmospheric potassium layer were performed on the German research vessel Polarstern from March to June 1996. K density profiles were obtained between 71°S and 45°N. The nightly mean peak densities ranged from 140 cm−3 in the equatorial region to 10 cm−3 in the Antarctic, and the column abundances decreased from 1.2 × 108 to 1.3 × 107 cm−2 going from low to high latitudes. High peak densities and column abundances were also commonly observed together with sporadic K layers. The global mean peak height of the normal (background) K layer was found to be 88.3 km. After the Polarstern campaign, observations were continued at Kühlungsborn (54°N). The summer and winter K layers, observed during July 1996 and January 1997, were quite different in shape but had similar peak densities and column abundances. A one‐dimensional model of the K layer was developed which includes meteoric deposition, vertical transport through eddy diffusion, and a full chemical scheme. This model was able to reproduce very satisfactorily the seasonal behavior of the K layer at 54°N if the wintertime deposition flux of the metal was reduced by 30% compared to the summer. The midlatitude ratio of K to Na was about 1%, much less than either the chondritic or cosmic ratios of the two metals (≈8 or 6%, respectively). The most likely reason is that potassium vaporizes less efficiently from meteoroids than sodium, in agreement with a thermodynamic model of a nonideal chondritic magma and observations in the exosphere of Mercury. Finally, the model was generally very successful in reproducing the latitudinal variations in the K layer.