Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake
Total electron content (TEC) data obtained from receivers of global navigation satellite systems (GNSSs) are increasingly being used to detect pre-earthquake ionospheric anomalies. In this study, the pre-earthquake ionospheric anomalies that occurred before the 2010 Baja California (32.128° N, 115.3...
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Online Access: | http://dx.doi.org/10.1080/19475705.2016.1208684 |
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doaj-4910ee00d8c34bde9f91a2108d24fe972020-11-25T01:28:53ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132017-12-018229530810.1080/19475705.2016.12086841208684Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquakeMustafa Ulukavak0Mualla Yalcinkaya1Karadeniz Technical UniversityKaradeniz Technical UniversityTotal electron content (TEC) data obtained from receivers of global navigation satellite systems (GNSSs) are increasingly being used to detect pre-earthquake ionospheric anomalies. In this study, the pre-earthquake ionospheric anomalies that occurred before the 2010 Baja California (32.128° N, 115.303° W, 4 April 2010, 22:40:42 UTC, Mw = 7.2) earthquake were investigated using TEC from Global Positioning System–Total Electron Content (GPS-TEC) data from five International GNSS Service (IGS) stations (SIO3, GOL2, QUIN, AMC2 and DRAO) near the epicentre and one IGS station (GRAZ) away from the epicentre. An analysis of the time of occurrence and duration yielded the following conclusions: both positive and negative anomalies are likely to occur and earthquake-related ionospheric anomalies occurred one to five days before the associated earthquake. The potential causes of these results were discussed. The observed anomalous variations in GPS-TEC may be attributed to the earthquake.http://dx.doi.org/10.1080/19475705.2016.1208684earthquakebaja californiatotal electron content (tec)gnssionosphere |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mustafa Ulukavak Mualla Yalcinkaya |
spellingShingle |
Mustafa Ulukavak Mualla Yalcinkaya Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake Geomatics, Natural Hazards & Risk earthquake baja california total electron content (tec) gnss ionosphere |
author_facet |
Mustafa Ulukavak Mualla Yalcinkaya |
author_sort |
Mustafa Ulukavak |
title |
Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake |
title_short |
Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake |
title_full |
Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake |
title_fullStr |
Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake |
title_full_unstemmed |
Precursor analysis of ionospheric GPS-TEC variations before the 2010 M7.2 Baja California earthquake |
title_sort |
precursor analysis of ionospheric gps-tec variations before the 2010 m7.2 baja california earthquake |
publisher |
Taylor & Francis Group |
series |
Geomatics, Natural Hazards & Risk |
issn |
1947-5705 1947-5713 |
publishDate |
2017-12-01 |
description |
Total electron content (TEC) data obtained from receivers of global navigation satellite systems (GNSSs) are increasingly being used to detect pre-earthquake ionospheric anomalies. In this study, the pre-earthquake ionospheric anomalies that occurred before the 2010 Baja California (32.128° N, 115.303° W, 4 April 2010, 22:40:42 UTC, Mw = 7.2) earthquake were investigated using TEC from Global Positioning System–Total Electron Content (GPS-TEC) data from five International GNSS Service (IGS) stations (SIO3, GOL2, QUIN, AMC2 and DRAO) near the epicentre and one IGS station (GRAZ) away from the epicentre. An analysis of the time of occurrence and duration yielded the following conclusions: both positive and negative anomalies are likely to occur and earthquake-related ionospheric anomalies occurred one to five days before the associated earthquake. The potential causes of these results were discussed. The observed anomalous variations in GPS-TEC may be attributed to the earthquake. |
topic |
earthquake baja california total electron content (tec) gnss ionosphere |
url |
http://dx.doi.org/10.1080/19475705.2016.1208684 |
work_keys_str_mv |
AT mustafaulukavak precursoranalysisofionosphericgpstecvariationsbeforethe2010m72bajacaliforniaearthquake AT muallayalcinkaya precursoranalysisofionosphericgpstecvariationsbeforethe2010m72bajacaliforniaearthquake |
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