Analysis of ionosphere changes due to earthquakes (case study: Regency of Lombok and Donggala)

M. N. Cahyadi; M. T.A. Prasetyo

doi:10.1088/1755-1315/389/1/012044

Analysis of ionosphere changes due to earthquakes (case study: Regency of Lombok and Donggala)

M. N. Cahyadi
, M. T.A. Prasetyo

Institut Teknologi Sepuluh Nopember

Research output: Contribution to journal › Conference article › peer-review

1 Citation (Scopus)

Abstract

Earthquakes will form and propagate atmospheric waves, rayleigh waves, acoustic waves and gravity waves. When acoustic waves reach the ionosphere, this affects the ionospheric electron density that can be known from GNSS signals, this disorder is commonly called CID. Electromagnetic waves transmitted by GPS satellite signals that pass through the ionosphere will cause a delay in time, from this data can be used to detect the presence of ionospheric variations through TEC values. In this study an analysis of ionospheric changes due to the earthquake that occurred in Lombok Regency and Donggala Regency. The result of the analysis show that the value of ionospheric disturbance from 5 August-28 September 2018 was around 0.19 TECU-0.56 TECU.

Original language	English
Article number	012044
Journal	IOP Conference Series: Earth and Environmental Science
Volume	389
Issue number	1
DOIs	https://doi.org/10.1088/1755-1315/389/1/012044
Publication status	Published - 13 Dec 2019
Event	4th Geomatics International Conference 2019, GeoICON 2019 - Surabaya, Indonesia Duration: 21 Aug 2019 → 22 Aug 2019

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10.1088/1755-1315/389/1/012044

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title = "Analysis of ionosphere changes due to earthquakes (case study: Regency of Lombok and Donggala)",

abstract = "Earthquakes will form and propagate atmospheric waves, rayleigh waves, acoustic waves and gravity waves. When acoustic waves reach the ionosphere, this affects the ionospheric electron density that can be known from GNSS signals, this disorder is commonly called CID. Electromagnetic waves transmitted by GPS satellite signals that pass through the ionosphere will cause a delay in time, from this data can be used to detect the presence of ionospheric variations through TEC values. In this study an analysis of ionospheric changes due to the earthquake that occurred in Lombok Regency and Donggala Regency. The result of the analysis show that the value of ionospheric disturbance from 5 August-28 September 2018 was around 0.19 TECU-0.56 TECU.",

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T1 - Analysis of ionosphere changes due to earthquakes (case study: Regency of Lombok and Donggala)

AU - Cahyadi, M. N.

AU - Prasetyo, M. T.A.

PY - 2019/12/13

Y1 - 2019/12/13

N2 - Earthquakes will form and propagate atmospheric waves, rayleigh waves, acoustic waves and gravity waves. When acoustic waves reach the ionosphere, this affects the ionospheric electron density that can be known from GNSS signals, this disorder is commonly called CID. Electromagnetic waves transmitted by GPS satellite signals that pass through the ionosphere will cause a delay in time, from this data can be used to detect the presence of ionospheric variations through TEC values. In this study an analysis of ionospheric changes due to the earthquake that occurred in Lombok Regency and Donggala Regency. The result of the analysis show that the value of ionospheric disturbance from 5 August-28 September 2018 was around 0.19 TECU-0.56 TECU.

AB - Earthquakes will form and propagate atmospheric waves, rayleigh waves, acoustic waves and gravity waves. When acoustic waves reach the ionosphere, this affects the ionospheric electron density that can be known from GNSS signals, this disorder is commonly called CID. Electromagnetic waves transmitted by GPS satellite signals that pass through the ionosphere will cause a delay in time, from this data can be used to detect the presence of ionospheric variations through TEC values. In this study an analysis of ionospheric changes due to the earthquake that occurred in Lombok Regency and Donggala Regency. The result of the analysis show that the value of ionospheric disturbance from 5 August-28 September 2018 was around 0.19 TECU-0.56 TECU.

UR - https://www.scopus.com/pages/publications/85077629915

U2 - 10.1088/1755-1315/389/1/012044

DO - 10.1088/1755-1315/389/1/012044

M3 - Conference article

AN - SCOPUS:85077629915

SN - 1755-1307

VL - 389

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

IS - 1

M1 - 012044

T2 - 4th Geomatics International Conference 2019, GeoICON 2019

Y2 - 21 August 2019 through 22 August 2019

ER -

Analysis of ionosphere changes due to earthquakes (case study: Regency of Lombok and Donggala)

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