Changes of neutral composition in the thermosphere

A. G. Burns, T. L. Killeen

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

Neutral thermotropic composition changes in response to several external inputs. Solar EUV radiation is absorbed throughout this region, and upward propagating tides and gravity waves are particularly important in the lower thermosphere. Coupling between the magnetosphere and the thermosphere/ionosphere system also affects neutral composition, both through the effects of joule heating and horizontal transport by ion-neutral momentum transfer. The major feature of these changes in composition at 300 km is the large enhancement of N2 density that occur over the magnetic polar cap within minutes to hours after the onset of the storm. These N2 enhancements can extend to low latitudes. Other changes in neutral composition include enhanced oxygen and NO densities, relative to N2 densities.

Original languageEnglish (US)
Title of host publicationAstrodynamics 1991
PublisherPubl by Univelt Inc
Pages2295-2311
Number of pages17
Editionpt 3
ISBN (Print)0877033471
StatePublished - Jan 1 1992
Externally publishedYes
EventProceedings of the AAS/AIAA Astrodynamics Conference - Durango, CO, USA
Duration: Aug 19 1991Aug 22 1991

Publication series

NameAdvances in the Astronautical Sciences
Numberpt 3
Volume76
ISSN (Print)0065-3438

Other

OtherProceedings of the AAS/AIAA Astrodynamics Conference
CityDurango, CO, USA
Period8/19/918/22/91

ASJC Scopus subject areas

  • Aerospace Engineering
  • Space and Planetary Science

Fingerprint

Dive into the research topics of 'Changes of neutral composition in the thermosphere'. Together they form a unique fingerprint.

Cite this