Time‐varying ionosonde trend: Case study of Sodankylä hmF2 data 1957–2014. Issue 8 (13th August 2015)

• Record Type: Journal Article
• Authors: Roininen, Lassi; Laine, Marko; Ulich, Thomas
• Is Part Of: Journal of geophysical research. Volume 120:Issue 8(2015:Aug.)
• Page Start: 6851
• Page End: 6859
• Publication Date: 2015-08-13
• Subjects: Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1002/2015JA021176
• Languages: English
• ISSNs: 2169-9380

Abstract

<abstract abstract-type="main" id="jgra51960-abs-0001"> <title>Abstract</title> <p id="jgra51960-para-0001">We discuss trend analysis of nonstationary ionosonde <italic>h</italic><sub><italic>m</italic></sub><italic>F</italic><sub>2</sub> time series measured at Sodankylä Geophysical Observatory (67.4<sup>∘</sup>N, 26.7<sup>∘</sup>E), Finland, 1957–2014. We model the <italic>h</italic><sub><italic>m</italic></sub><italic>F</italic><sub>2</sub> with a dynamic regression time series model with the following components: a slowly varying background level, seasonal variations, and solar effects. We analyze the time series with a dynamic linear state space model. Such an approach allows model components to vary in time, allowing us to study the dynamic stochastic nature of the underlying long‐term trend. This feature is lacking in most time series models used in atmospheric and environmental long‐term trend analyses. Our objective is to understand the long‐term <italic>h</italic><sub><italic>m</italic></sub><italic>F</italic><sub>2</sub> trend with respect to increased levels of carbon dioxide and methane in the atmosphere. Based on model estimates, this phenomenon is predicted to cool the thermosphere and leads to decrease of the altitude of the so‐called <italic>F</italic><sub>2</sub> layer peak. After accounting for the effects of solar activity variations on the data, we see that the estimated trend shows an almost 30 km decrease of the <italic>F</italic><sub>2</sub> layer peak during the observation period. The decrease of the peak during 1990–2010 is significantly greater than during earlier observation period.</p> </abstract>