Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance

Several currently operating instruments are able to measure the full EUV spectrum at sufficient wavelength resolution for use in upper-atmosphere modeling, the effects of space weather, and modeling satellite drag. However, no missions are planned at present to succeed the Thermosphere Ionosphere Me...

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Main Authors: Suess Katherine, Snow Martin, Viereck Rodney, Machol Janet
Format: Article
Language:English
Published: EDP Sciences 2016-01-01
Series:Journal of Space Weather and Space Climate
Subjects:
Online Access:http://dx.doi.org/10.1051/swsc/2016003
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spelling doaj-45236dc20fbf434b99b540212d431b342021-02-02T02:53:33ZengEDP SciencesJournal of Space Weather and Space Climate2115-72512016-01-016A1010.1051/swsc/2016003swsc150034Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradianceSuess KatherineSnow MartinViereck RodneyMachol JanetSeveral currently operating instruments are able to measure the full EUV spectrum at sufficient wavelength resolution for use in upper-atmosphere modeling, the effects of space weather, and modeling satellite drag. However, no missions are planned at present to succeed the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) and Solar Dynamics Observatory (SDO) missions, which currently provide these data sources. To develop a suitable replacement for these measurements, we use two broadband EUV channels on the NOAA GOES satellites, the magnesium core-to-wing ratio (Mg II index) from the SOlar Radiation and Climate Experiment (SORCE) as well as EUV and Mg II time averages to model the EUV spectrum from 0.1 to 105 nm at 5-nm spectral resolution and daily time resolution. A Levenberg-Marquardt least squares fitting algorithm is used to determine a coefficient matrix that best reproduces a reference data set when multiplied by input data. The coefficient matrix is then applied to model data outside of the fitting interval. Three different fitting intervals are tested, with a variable fitting interval utilizing all days of data before the prediction date producing the best results. The correlation between the model results and the observed spectrum is found to be above 95% for the 0.1–50 nm range, and between 74% and 95% for the 50–105 nm range. We also find a favorable comparison between our results and the Flare Irradiance Spectral Model (FISM). These results provide a promising potential source for an empirical EUV spectral model after direct EUV measurements are no longer available, and utilize a similar EUV modeling technique as the upcoming GOES-R satellites.http://dx.doi.org/10.1051/swsc/2016003Solar irradianceEUV fluxSpace weather
collection DOAJ
language English
format Article
sources DOAJ
author Suess Katherine
Snow Martin
Viereck Rodney
Machol Janet
spellingShingle Suess Katherine
Snow Martin
Viereck Rodney
Machol Janet
Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
Journal of Space Weather and Space Climate
Solar irradiance
EUV flux
Space weather
author_facet Suess Katherine
Snow Martin
Viereck Rodney
Machol Janet
author_sort Suess Katherine
title Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
title_short Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
title_full Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
title_fullStr Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
title_full_unstemmed Solar Spectral Proxy Irradiance from GOES (SSPRING): a model for solar EUV irradiance
title_sort solar spectral proxy irradiance from goes (sspring): a model for solar euv irradiance
publisher EDP Sciences
series Journal of Space Weather and Space Climate
issn 2115-7251
publishDate 2016-01-01
description Several currently operating instruments are able to measure the full EUV spectrum at sufficient wavelength resolution for use in upper-atmosphere modeling, the effects of space weather, and modeling satellite drag. However, no missions are planned at present to succeed the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) and Solar Dynamics Observatory (SDO) missions, which currently provide these data sources. To develop a suitable replacement for these measurements, we use two broadband EUV channels on the NOAA GOES satellites, the magnesium core-to-wing ratio (Mg II index) from the SOlar Radiation and Climate Experiment (SORCE) as well as EUV and Mg II time averages to model the EUV spectrum from 0.1 to 105 nm at 5-nm spectral resolution and daily time resolution. A Levenberg-Marquardt least squares fitting algorithm is used to determine a coefficient matrix that best reproduces a reference data set when multiplied by input data. The coefficient matrix is then applied to model data outside of the fitting interval. Three different fitting intervals are tested, with a variable fitting interval utilizing all days of data before the prediction date producing the best results. The correlation between the model results and the observed spectrum is found to be above 95% for the 0.1–50 nm range, and between 74% and 95% for the 50–105 nm range. We also find a favorable comparison between our results and the Flare Irradiance Spectral Model (FISM). These results provide a promising potential source for an empirical EUV spectral model after direct EUV measurements are no longer available, and utilize a similar EUV modeling technique as the upcoming GOES-R satellites.
topic Solar irradiance
EUV flux
Space weather
url http://dx.doi.org/10.1051/swsc/2016003
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AT viereckrodney solarspectralproxyirradiancefromgoessspringamodelforsolareuvirradiance
AT macholjanet solarspectralproxyirradiancefromgoessspringamodelforsolareuvirradiance
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