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...

Full description

Bibliographic Details
Main Authors: Mustafa Ulukavak, Mualla Yalcinkaya
Format: Article
Language:English
Published: Taylor & Francis Group 2017-12-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:http://dx.doi.org/10.1080/19475705.2016.1208684
id doaj-4910ee00d8c34bde9f91a2108d24fe97
record_format Article
spelling 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
_version_ 1725099710373429248