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The Response of the Equatorial Ionosphere over Nigeria to a Geomagnetic Storm Event
The total electron content (TEC) data obtained from the ground-based GPS receiver stations of the Nigerian GNSS network of stations (NIGNET) have been used in this study to analyse the response of equatorial and low-latitude ionosphere to strong geomagnetic storms that occurred on October 25, 2011....
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Published in: | Geomagnetism and Aeronomy 2021-07, Vol.61 (4), p.647-657 |
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container_title | Geomagnetism and Aeronomy |
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creator | Akinyemi, G. A. Kolawole, L. B. Dairo, O. F. Willoughby, A. A. Abdulrahim, R. B. Rabiu, A. B. |
description | The total electron content (TEC) data obtained from the ground-based GPS receiver stations of the Nigerian GNSS network of stations (NIGNET) have been used in this study to analyse the response of equatorial and low-latitude ionosphere to strong geomagnetic storms that occurred on October 25, 2011. The stations and their respective geomagnetic latitudes are Lagos (−3
.
03°), Yola (−1
.
32°) and Birnin Kebbi (0
.
72°). The storm caused enhancements in TEC (positive storm effect) in comparison with the quiet condition’s TEC across all the stations during both the main and the recovery phases. During the storm of October 25, recorded maximum enhancements in TEC were 181.86%, 142.34% and 181.24% in Kebbi, Yola and Lagos respectively.The magnitude of the ionospheric irregularities was higher at the night (October 25) of the main phase of the geomagnetic storm than the night (October 24) before the storm onset. |
doi_str_mv | 10.1134/S0016793221040022 |
format | article |
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.
03°), Yola (−1
.
32°) and Birnin Kebbi (0
.
72°). The storm caused enhancements in TEC (positive storm effect) in comparison with the quiet condition’s TEC across all the stations during both the main and the recovery phases. During the storm of October 25, recorded maximum enhancements in TEC were 181.86%, 142.34% and 181.24% in Kebbi, Yola and Lagos respectively.The magnitude of the ionospheric irregularities was higher at the night (October 25) of the main phase of the geomagnetic storm than the night (October 24) before the storm onset.</description><identifier>ISSN: 0016-7932</identifier><identifier>EISSN: 1555-645X</identifier><identifier>EISSN: 0016-7940</identifier><identifier>DOI: 10.1134/S0016793221040022</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Equatorial ionosphere ; Geomagnetic storms ; Geomagnetism ; Geophysics/Geodesy ; Global positioning systems ; GPS ; Ionosphere ; Ionospheric irregularities ; Latitude ; Magnetic storms ; Night ; Satellite navigation systems ; Storm effects ; Storms ; Total Electron Content</subject><ispartof>Geomagnetism and Aeronomy, 2021-07, Vol.61 (4), p.647-657</ispartof><rights>Pleiades Publishing, Ltd. 2021. ISSN 0016-7932, Geomagnetism and Aeronomy, 2021, Vol. 61, No. 4, pp. 647–657. © Pleiades Publishing, Ltd., 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-6729ef5d706669e430807c16eb81247683e5fac3f168144095f4a476070a48b83</citedby><cites>FETCH-LOGICAL-c316t-6729ef5d706669e430807c16eb81247683e5fac3f168144095f4a476070a48b83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Akinyemi, G. A.</creatorcontrib><creatorcontrib>Kolawole, L. B.</creatorcontrib><creatorcontrib>Dairo, O. F.</creatorcontrib><creatorcontrib>Willoughby, A. A.</creatorcontrib><creatorcontrib>Abdulrahim, R. B.</creatorcontrib><creatorcontrib>Rabiu, A. B.</creatorcontrib><title>The Response of the Equatorial Ionosphere over Nigeria to a Geomagnetic Storm Event</title><title>Geomagnetism and Aeronomy</title><addtitle>Geomagn. Aeron</addtitle><description>The total electron content (TEC) data obtained from the ground-based GPS receiver stations of the Nigerian GNSS network of stations (NIGNET) have been used in this study to analyse the response of equatorial and low-latitude ionosphere to strong geomagnetic storms that occurred on October 25, 2011. The stations and their respective geomagnetic latitudes are Lagos (−3
.
03°), Yola (−1
.
32°) and Birnin Kebbi (0
.
72°). The storm caused enhancements in TEC (positive storm effect) in comparison with the quiet condition’s TEC across all the stations during both the main and the recovery phases. During the storm of October 25, recorded maximum enhancements in TEC were 181.86%, 142.34% and 181.24% in Kebbi, Yola and Lagos respectively.The magnitude of the ionospheric irregularities was higher at the night (October 25) of the main phase of the geomagnetic storm than the night (October 24) before the storm onset.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Equatorial ionosphere</subject><subject>Geomagnetic storms</subject><subject>Geomagnetism</subject><subject>Geophysics/Geodesy</subject><subject>Global positioning systems</subject><subject>GPS</subject><subject>Ionosphere</subject><subject>Ionospheric irregularities</subject><subject>Latitude</subject><subject>Magnetic storms</subject><subject>Night</subject><subject>Satellite navigation systems</subject><subject>Storm effects</subject><subject>Storms</subject><subject>Total Electron Content</subject><issn>0016-7932</issn><issn>1555-645X</issn><issn>0016-7940</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kE9Lw0AQxRdRsFY_gLcFz9HZ_5ujlFoLRcFW8Ba2cdKmtNl0Nyn47d1SwYN4GmZ-780wj5BbBveMCfkwB2Da5IJzBhKA8zMyYEqpTEv1cU4GR5wd-SW5inEDIEApNiDzxRrpG8bWNxGpr2iX-vG-d50PtdvSqW98bNcYEjxgoC_1ChOgnaeOTtDv3KrBri7pPBl2dHzAprsmF5XbRrz5qUPy_jRejJ6z2etkOnqcZaVgusu04TlW6tOA1jpHKcCCKZnGpWVcGm0FqsqVomLaMikhV5V0aQ4GnLRLK4bk7rS3DX7fY-yKje9Dk04WXGnLjQJtkoqdVGXwMQasijbUOxe-CgbFMbviT3bJw0-emLRN-vh38_-mb5mnbgw</recordid><startdate>20210701</startdate><enddate>20210701</enddate><creator>Akinyemi, G. A.</creator><creator>Kolawole, L. B.</creator><creator>Dairo, O. F.</creator><creator>Willoughby, A. A.</creator><creator>Abdulrahim, R. B.</creator><creator>Rabiu, A. B.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope></search><sort><creationdate>20210701</creationdate><title>The Response of the Equatorial Ionosphere over Nigeria to a Geomagnetic Storm Event</title><author>Akinyemi, G. A. ; Kolawole, L. B. ; Dairo, O. F. ; Willoughby, A. A. ; Abdulrahim, R. B. ; Rabiu, A. B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-6729ef5d706669e430807c16eb81247683e5fac3f168144095f4a476070a48b83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Equatorial ionosphere</topic><topic>Geomagnetic storms</topic><topic>Geomagnetism</topic><topic>Geophysics/Geodesy</topic><topic>Global positioning systems</topic><topic>GPS</topic><topic>Ionosphere</topic><topic>Ionospheric irregularities</topic><topic>Latitude</topic><topic>Magnetic storms</topic><topic>Night</topic><topic>Satellite navigation systems</topic><topic>Storm effects</topic><topic>Storms</topic><topic>Total Electron Content</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Akinyemi, G. A.</creatorcontrib><creatorcontrib>Kolawole, L. B.</creatorcontrib><creatorcontrib>Dairo, O. F.</creatorcontrib><creatorcontrib>Willoughby, A. A.</creatorcontrib><creatorcontrib>Abdulrahim, R. B.</creatorcontrib><creatorcontrib>Rabiu, A. B.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geomagnetism and Aeronomy</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Akinyemi, G. A.</au><au>Kolawole, L. B.</au><au>Dairo, O. F.</au><au>Willoughby, A. A.</au><au>Abdulrahim, R. B.</au><au>Rabiu, A. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Response of the Equatorial Ionosphere over Nigeria to a Geomagnetic Storm Event</atitle><jtitle>Geomagnetism and Aeronomy</jtitle><stitle>Geomagn. Aeron</stitle><date>2021-07-01</date><risdate>2021</risdate><volume>61</volume><issue>4</issue><spage>647</spage><epage>657</epage><pages>647-657</pages><issn>0016-7932</issn><eissn>1555-645X</eissn><eissn>0016-7940</eissn><abstract>The total electron content (TEC) data obtained from the ground-based GPS receiver stations of the Nigerian GNSS network of stations (NIGNET) have been used in this study to analyse the response of equatorial and low-latitude ionosphere to strong geomagnetic storms that occurred on October 25, 2011. The stations and their respective geomagnetic latitudes are Lagos (−3
.
03°), Yola (−1
.
32°) and Birnin Kebbi (0
.
72°). The storm caused enhancements in TEC (positive storm effect) in comparison with the quiet condition’s TEC across all the stations during both the main and the recovery phases. During the storm of October 25, recorded maximum enhancements in TEC were 181.86%, 142.34% and 181.24% in Kebbi, Yola and Lagos respectively.The magnitude of the ionospheric irregularities was higher at the night (October 25) of the main phase of the geomagnetic storm than the night (October 24) before the storm onset.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016793221040022</doi><tpages>11</tpages></addata></record> |
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subjects | Earth and Environmental Science Earth Sciences Equatorial ionosphere Geomagnetic storms Geomagnetism Geophysics/Geodesy Global positioning systems GPS Ionosphere Ionospheric irregularities Latitude Magnetic storms Night Satellite navigation systems Storm effects Storms Total Electron Content |
title | The Response of the Equatorial Ionosphere over Nigeria to a Geomagnetic Storm Event |
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