Determining long-term change in the ionosphere

Eos

Volumn 84, Issue 52, 2003, Pages

  Ulich, Thomas ^a   Culverd, Mark A ^b   Rishbeth, Henry ^c  

^a UNIVERSITY OF OULU   (Finland)

^b BRITISH ANTARCTIC SURVEY   (United Kingdom)

^c UNIVERSITY OF SOUTHAMPTON   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 8844270590     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2003EO520002     Document Type: Article

References (10)

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3. Clilverd,M.A.,T. Ulich, and M.J.Jarvis, Residual solar cycle influence on trends in ionospheric F2-layer peak height,J Geophys. Res., 108,A12, 1450,10.1029/ 2003JA009838, 2003.
4. Dudeney.J.R.,A simple empirical method for estimating the height and semithickness of the P2-layer at the Argentine Islands, Graham L.and,Scientific Reports 88, British Antarctic Survey, Cambridge, U.K., 1974.
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7. Roble, R. G.,and R. E. Dickinson, How will changes in carbon dioxide and methane modify the mean structure of the mesosphere and thermosphere, Geophys. Res. Left, 16,1441-1444,1989.
8. Shimazaki,T.,World-wide variations in the height of the maximum electron density of the ionospheric F2 layer,J Radio Res. Labs Japan, 2, 85-97, 1955.
9. Ulich,T, and E.Turunen, Evidence for long-term cooling of the upper atmosphere in lonosonde data, Geop !zys. Res. Left., 24,1103-1106,1997.
10. Weatherhead, E. C., et al., Factors affecting the detection of trends: Statistical considerations and applications to environmental data,J Geophys. Res., 103,17149 17161,1998.