Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001

Using digital ionosonde observations at a low mid-latitude station, New Delhi (28.6°N, 77.2°E, dip 42.4°N), we have derived hourly monthly values of <i>hm</i>F2 (the real height corresponding to the peak electron density in the F2-region), employing both the Dudeney&nbsp;(1983) a...

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Main Authors: N. K. Sethi, R. S. Dabas, V. K. Vohra
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/453/2004/angeo-22-453-2004.pdf
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spelling doaj-2564e38b00cc434e8570f59de71a03022020-11-25T00:51:36ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-01-012245345810.5194/angeo-22-453-2004Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001N. K. Sethi0R. S. Dabas1V. K. Vohra2Radio and Atmospheric Sciences Division, National Physical Laboratory, Dr. K. S. Krishnan Road, New Delhi, 110 012, IndiaRadio and Atmospheric Sciences Division, National Physical Laboratory, Dr. K. S. Krishnan Road, New Delhi, 110 012, IndiaRadio and Atmospheric Sciences Division, National Physical Laboratory, Dr. K. S. Krishnan Road, New Delhi, 110 012, IndiaUsing digital ionosonde observations at a low mid-latitude station, New Delhi (28.6°N, 77.2°E, dip 42.4°N), we have derived hourly monthly values of <i>hm</i>F2 (the real height corresponding to the peak electron density in the F2-region), employing both the Dudeney&nbsp;(1983) and Bilitza&nbsp;(1990) empirical formulations for the period from January 2001 to August 2002. The diurnal and seasonal variations of <i>hm</i>F2 are analyzed. Further, to assess the predictability of the latest available model, International Reference Ionosphere, (IRI-2001), we have obtained the median values of <i>hm</i>F2 derived from M(3000)F2 for each hour during different seasons and compare these with the model. Our results show that both the Dudeney&nbsp;(1983) and Bilitza (1990) formulations reveal more or less a similar diurnal trend of <i>hm</i>F2, with higher values around midnight and lower during sunrise, in all the seasons. It is also noted that the <i>hm</i>F2 shows a larger variability around midnight than by daytime, in all the seasons. Further, the study shows that median values of observed <i>hm</i>F2, using both formulations, are somewhat larger than those predicted by the IRI, in all seasons and at all local times. During summer, the IRI values agree comparatively well with the observations, especially during daytime. Major discrepancies occur when the IRI underestimates observed <i>hm</i>F2 for local times from about 14:00&nbsp;LT to 18:00&nbsp;LT and 04:00&nbsp;LT to 05:00&nbsp;LT during winter and equinox, where the percentage deviation of the observed <i>hm</i>F2 values with respect to the IRI model varies from 15 to 25%. The difference between the model and observations, outside this time period, remains less than 20% during all the seasons.<br><br> <b>Key words.</b> Ionosphere (modelling and forecasting; equatorial ionosphere)https://www.ann-geophys.net/22/453/2004/angeo-22-453-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. K. Sethi
R. S. Dabas
V. K. Vohra
spellingShingle N. K. Sethi
R. S. Dabas
V. K. Vohra
Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
Annales Geophysicae
author_facet N. K. Sethi
R. S. Dabas
V. K. Vohra
author_sort N. K. Sethi
title Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
title_short Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
title_full Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
title_fullStr Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
title_full_unstemmed Diurnal and seasonal variations of <i>hm</i>F2 deduced from digitalionosonde over New Delhi and its comparison with IRI 2001
title_sort diurnal and seasonal variations of <i>hm</i>f2 deduced from digitalionosonde over new delhi and its comparison with iri 2001
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2004-01-01
description Using digital ionosonde observations at a low mid-latitude station, New Delhi (28.6°N, 77.2°E, dip 42.4°N), we have derived hourly monthly values of <i>hm</i>F2 (the real height corresponding to the peak electron density in the F2-region), employing both the Dudeney&nbsp;(1983) and Bilitza&nbsp;(1990) empirical formulations for the period from January 2001 to August 2002. The diurnal and seasonal variations of <i>hm</i>F2 are analyzed. Further, to assess the predictability of the latest available model, International Reference Ionosphere, (IRI-2001), we have obtained the median values of <i>hm</i>F2 derived from M(3000)F2 for each hour during different seasons and compare these with the model. Our results show that both the Dudeney&nbsp;(1983) and Bilitza (1990) formulations reveal more or less a similar diurnal trend of <i>hm</i>F2, with higher values around midnight and lower during sunrise, in all the seasons. It is also noted that the <i>hm</i>F2 shows a larger variability around midnight than by daytime, in all the seasons. Further, the study shows that median values of observed <i>hm</i>F2, using both formulations, are somewhat larger than those predicted by the IRI, in all seasons and at all local times. During summer, the IRI values agree comparatively well with the observations, especially during daytime. Major discrepancies occur when the IRI underestimates observed <i>hm</i>F2 for local times from about 14:00&nbsp;LT to 18:00&nbsp;LT and 04:00&nbsp;LT to 05:00&nbsp;LT during winter and equinox, where the percentage deviation of the observed <i>hm</i>F2 values with respect to the IRI model varies from 15 to 25%. The difference between the model and observations, outside this time period, remains less than 20% during all the seasons.<br><br> <b>Key words.</b> Ionosphere (modelling and forecasting; equatorial ionosphere)
url https://www.ann-geophys.net/22/453/2004/angeo-22-453-2004.pdf
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