Trends in foF2 above Tromsø (69°N 19°E)

C. M. Hall; P. S. Cannon

doi:10.1029/2002GL016259

Trends in foF2 above Tromsø (69°N 19°E)

C. M. Hall, P. S. Cannon

Electronic, Electrical and Systems Engineering

Research output: Contribution to journal › Article › peer-review

20 Citations (Scopus)

Abstract

Regular ionosonde observations from Tromsø (69°N 19°E) date from 1935 and the dataset thus represents one of the longest in existence. Trends in the critical frequency of the ionospheric F2 layer are determined and found to be negative. Our results lend support to a causative mechanism which includes greenhouse cooling.

Original language	English
Article number	2128
Journal	Geophysical Research Letters
Volume	29
Issue number	23
DOIs	https://doi.org/10.1029/2002GL016259
Publication status	Published - 1 Dec 2002

Bibliographical note

Publisher Copyright:
© Copyright 2002 by the American Geophysical Union.

ASJC Scopus subject areas

Geophysics
General Earth and Planetary Sciences

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10.1029/2002GL016259

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abstract = "Regular ionosonde observations from Troms{\o} (69°N 19°E) date from 1935 and the dataset thus represents one of the longest in existence. Trends in the critical frequency of the ionospheric F2 layer are determined and found to be negative. Our results lend support to a causative mechanism which includes greenhouse cooling.",

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AB - Regular ionosonde observations from Tromsø (69°N 19°E) date from 1935 and the dataset thus represents one of the longest in existence. Trends in the critical frequency of the ionospheric F2 layer are determined and found to be negative. Our results lend support to a causative mechanism which includes greenhouse cooling.

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Trends in foF2 above Tromsø (69°N 19°E)

Abstract

Bibliographical note

ASJC Scopus subject areas

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