Climatic trends in E-region critical frequency and virtual height above Tromsø (70° N, 10° E)

We have examined the long time series of observations of E-region virtual height (1948–2006) and critical frequency (1935-2006) hitherto made by the Tromsø ionosonde at 70° N, 19° E. Combining a simplistic trend analysis with a rigorous treatment of errors we identify a...

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Bibliographic Details
Main Authors: C. M. Hall, A. Brekke, P. S. Cannon
Format: Article
Language:English
Published: Copernicus Publications 2007-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/25/2351/2007/angeo-25-2351-2007.pdf
Description
Summary:We have examined the long time series of observations of E-region virtual height (1948&ndash;2006) and critical frequency (1935-2006) hitherto made by the Tromsø ionosonde at 70&deg; N, 19&deg; E. Combining a simplistic trend analysis with a rigorous treatment of errors we identify a negative trend in critical frequency. While a similar analysis of the virtual height <i>h'E</i> also suggests a negative trend, a closer examination reveals a possible weak positive trend prior to ~1975 and a strong negative trend from ~1975 to present. These two metrics of essentially the same feature of the ionosphere do not exhibit the same signature since critical frequency is controlled by photochemistry within the E-layer while height is controlled by pressure level. We further find that the trend in critical frequency is a daylight/summer phenomenon, no significant trend being evident in the winter subset of the data. On the other hand, the trends in virtual height are independent of season/daylight.
ISSN:0992-7689
1432-0576