Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data

<p>Forecasting the thermosphere (the atmosphere's uppermost layer, from about 90 to 800&thinsp;km altitude) is crucial to space-related applications, from space mission design to re-entry operations, space surveillance and more. Thermospheric dynamics is directly linked to the solar...

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Main Authors: A. Bigazzi, C. Cauli, F. Berrilli
Format: Article
Language:English
Published: Copernicus Publications 2020-06-01
Series:Annales Geophysicae
Online Access:https://angeo.copernicus.org/articles/38/789/2020/angeo-38-789-2020.pdf
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spelling doaj-834bb307223847cd8e84f16ffd1570a62020-11-25T03:23:44ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762020-06-013878980010.5194/angeo-38-789-2020Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 dataA. BigazziC. CauliF. Berrilli<p>Forecasting the thermosphere (the atmosphere's uppermost layer, from about 90 to 800&thinsp;km altitude) is crucial to space-related applications, from space mission design to re-entry operations, space surveillance and more. Thermospheric dynamics is directly linked to the solar dynamics through the solar UV (ultraviolet) input, which is highly variable, and through the solar wind and plasma fluxes impacting Earth's magnetosphere. The solar input is non-periodic and non-stationary, with long-term modulations from the solar rotation and the solar cycle and impulsive components, due to magnetic storms. Proxies of the solar input exist and may be used to forecast the thermosphere, such as the F10.7 radio flux and the Mg II EUV (extreme-ultraviolet) flux. They relate to physical processes of the solar atmosphere. Other indices, such as the Ap geomagnetic index, connect with Earth's geomagnetic environment.</p> <p>We analyse the proxies' time series comparing them with in situ density data from the ESA (European Space Agency) GOCE (Gravity Field and Steady-State Ocean Circulation Explorer) gravity mission, operational from March 2009 to November 2013, therefore covering the full rising phase of solar cycle 24, exposing the entire dynamic range of the solar input. We use empirical mode decomposition (EMD), an analysis technique appropriate to non-periodic, multi-scale signals. Data are taken at an altitude of 260&thinsp;km, exceptionally low for a low-Earth-orbit (LEO) satellite, where density variations are the single most important perturbation to satellite dynamics.</p> <p>We show that the synthesized signal from optimally selected combinations of proxy basis functions, notably Mg II for the solar flux and Ap for the plasma component, shows a very good agreement with thermospheric data obtained by GOCE, during periods of low and medium solar activity. In periods of maximum solar activity, density enhancements are also well represented. The Mg II index proves to be, in general, a better proxy than the F10.7 index for modelling the solar flux because of its specific response to the UV spectrum, whose variations have the largest impact over thermospheric density.</p>https://angeo.copernicus.org/articles/38/789/2020/angeo-38-789-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Bigazzi
C. Cauli
F. Berrilli
spellingShingle A. Bigazzi
C. Cauli
F. Berrilli
Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
Annales Geophysicae
author_facet A. Bigazzi
C. Cauli
F. Berrilli
author_sort A. Bigazzi
title Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
title_short Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
title_full Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
title_fullStr Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
title_full_unstemmed Lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of GOCE 2009–2012 data
title_sort lower-thermosphere response to solar activity: an empirical-mode-decomposition analysis of goce 2009–2012 data
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2020-06-01
description <p>Forecasting the thermosphere (the atmosphere's uppermost layer, from about 90 to 800&thinsp;km altitude) is crucial to space-related applications, from space mission design to re-entry operations, space surveillance and more. Thermospheric dynamics is directly linked to the solar dynamics through the solar UV (ultraviolet) input, which is highly variable, and through the solar wind and plasma fluxes impacting Earth's magnetosphere. The solar input is non-periodic and non-stationary, with long-term modulations from the solar rotation and the solar cycle and impulsive components, due to magnetic storms. Proxies of the solar input exist and may be used to forecast the thermosphere, such as the F10.7 radio flux and the Mg II EUV (extreme-ultraviolet) flux. They relate to physical processes of the solar atmosphere. Other indices, such as the Ap geomagnetic index, connect with Earth's geomagnetic environment.</p> <p>We analyse the proxies' time series comparing them with in situ density data from the ESA (European Space Agency) GOCE (Gravity Field and Steady-State Ocean Circulation Explorer) gravity mission, operational from March 2009 to November 2013, therefore covering the full rising phase of solar cycle 24, exposing the entire dynamic range of the solar input. We use empirical mode decomposition (EMD), an analysis technique appropriate to non-periodic, multi-scale signals. Data are taken at an altitude of 260&thinsp;km, exceptionally low for a low-Earth-orbit (LEO) satellite, where density variations are the single most important perturbation to satellite dynamics.</p> <p>We show that the synthesized signal from optimally selected combinations of proxy basis functions, notably Mg II for the solar flux and Ap for the plasma component, shows a very good agreement with thermospheric data obtained by GOCE, during periods of low and medium solar activity. In periods of maximum solar activity, density enhancements are also well represented. The Mg II index proves to be, in general, a better proxy than the F10.7 index for modelling the solar flux because of its specific response to the UV spectrum, whose variations have the largest impact over thermospheric density.</p>
url https://angeo.copernicus.org/articles/38/789/2020/angeo-38-789-2020.pdf
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