Heat and momentum sources of mean circulation at an altitude of 70 to 100 km

Author:

EBEL A.

Publisher

Informa UK Limited

Subject

General Medicine

Reference21 articles.

1. On the meridional circulation in the presence of a steady state, symmetric, circumpolar vortex;Gilman;Tellus,1964

2. Seasonal variations of electron densities below 100 km at mid-latitudes-II. Electron densities and atmospheric circulation;Gregory;J. Atmosph. Terr. Phys.,1969

3. Wind models from 60 to 130 km altitude for different months and latitudes;Groves;J. Brit. Interplan. Soc.,1969

4. Groves, G. V. 1971. Atmospheric structure and its variations in the region from 25 to 120 km. AFCRL-71-0410, Environm. Res. Papers 368.

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1. The role of vertical momentum fluxes in maintaining global meridional circulation in the lower thermosphere/upper mesosphere;Journal of Atmospheric and Solar-Terrestrial Physics;1997-03

2. Momentum and heat sources of the mesosphere and lower thermosphere regions 70–110 km;Journal of Atmospheric and Terrestrial Physics;1995-07

3. Net radiative heating and diagnostics of the diabatic circulation in the 15–110 km height layer;Journal of Atmospheric and Terrestrial Physics;1994-10

4. Mean zonal acceleration and heating of the 70- to 100-km region;Journal of Geophysical Research: Space Physics;1991-02-01

5. Bibliography;Noctilucent Clouds;1989

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