A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions
An ionospheric forecasting empirical local model over Rome (IFELMOR) has been developed to predict the state of the critical frequency of the F2 layer (<I>fo</I>F2) during geomagnetic storms and disturbed ionospheric conditions. Hourly measurements of <I>fo</I>F2 obtained...
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doaj-439a20daad1f4cee88ade895dd408a2e2020-11-24T21:43:41ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-02-012632333410.5194/angeo-26-323-2008A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditionsM. Pietrella0L. Perrone1Istituto Nazionale di Geofisica e Vulcanologia, via di Vigna Murata 605, 00143 Rome, ItalyIstituto Nazionale di Geofisica e Vulcanologia, via di Vigna Murata 605, 00143 Rome, ItalyAn ionospheric forecasting empirical local model over Rome (IFELMOR) has been developed to predict the state of the critical frequency of the F2 layer (<I>fo</I>F2) during geomagnetic storms and disturbed ionospheric conditions. Hourly measurements of <I>fo</I>F2 obtained at the Rome observatory, hourly quiet-time values of <I>fo</I>F2 (<I>fo</I>F2<sub><I>QT</I></sub>), and the hourly time-weighted accumulation series derived from the geomagnetic planetary index <I>a<sub>p</sub></I> (<I>a<sub>p</sub></I>(τ)), were considered during the period January 1976–December 2003. Under the assumption that the ionospheric disturbance index log(<I>fo</I>F2/<I>fo</I>F2<sub><I>QT</I></sub>) is correlated to the integrated geomagnetic index <I>a<sub>p</sub></I>(τ), statistically significant regression coefficients are obtained for different months and for different ranges of <I>a<sub>p</sub></I>(τ) and used as input to calculate the short-term ionospheric forecasting of <I>fo</I>F2. The empirical storm-time ionospheric correction model (STORM) was used to make comparisons with the IFELMOR model. A few comparisons between STORM's performance, IFELMOR's performance, the median measurements and the <I>fo</I>F2<sub><I>QT</I></sub> values, were made for significant geomagnetic storm events (<I>a<sub>p</sub></I>>150) occurring from 2000 to 2003. The results provided by IFELMOR are satisfactory, in particular, for periods characterized by high geomagnetic activity and very disturbed ionospheric conditions.https://www.ann-geophys.net/26/323/2008/angeo-26-323-2008.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
M. Pietrella L. Perrone |
spellingShingle |
M. Pietrella L. Perrone A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions Annales Geophysicae |
author_facet |
M. Pietrella L. Perrone |
author_sort |
M. Pietrella |
title |
A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions |
title_short |
A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions |
title_full |
A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions |
title_fullStr |
A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions |
title_full_unstemmed |
A local ionospheric model for forecasting the critical frequency of the F2 layer during disturbed geomagnetic and ionospheric conditions |
title_sort |
local ionospheric model for forecasting the critical frequency of the f2 layer during disturbed geomagnetic and ionospheric conditions |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2008-02-01 |
description |
An ionospheric forecasting empirical local model over Rome (IFELMOR) has
been developed to predict the state of the critical frequency of the F2
layer (<I>fo</I>F2) during geomagnetic storms and disturbed ionospheric conditions.
Hourly measurements of <I>fo</I>F2 obtained at the Rome observatory, hourly
quiet-time values of <I>fo</I>F2 (<I>fo</I>F2<sub><I>QT</I></sub>), and the hourly time-weighted
accumulation series derived from the geomagnetic planetary index <I>a<sub>p</sub></I>
(<I>a<sub>p</sub></I>(τ)), were considered during the period January 1976–December
2003. Under the assumption that the ionospheric disturbance index log(<I>fo</I>F2/<I>fo</I>F2<sub><I>QT</I></sub>)
is correlated to the integrated geomagnetic index <I>a<sub>p</sub></I>(τ),
statistically significant regression coefficients are obtained for different
months and for different ranges of <I>a<sub>p</sub></I>(τ) and used as input to
calculate the short-term ionospheric forecasting of <I>fo</I>F2. The empirical
storm-time ionospheric correction model (STORM) was used to make comparisons
with the IFELMOR model. A few comparisons between STORM's performance,
IFELMOR's performance, the median measurements and the <I>fo</I>F2<sub><I>QT</I></sub> values,
were made for significant geomagnetic storm events (<I>a<sub>p</sub></I>>150) occurring
from 2000 to 2003. The results provided by IFELMOR are satisfactory, in
particular, for periods characterized by high geomagnetic activity and very
disturbed ionospheric conditions. |
url |
https://www.ann-geophys.net/26/323/2008/angeo-26-323-2008.pdf |
work_keys_str_mv |
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