A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission

The current work makes use of the geometrical configuration of the two lower-altitude Swarm satellites (Swarm A and C), moving side by side with a longitudinal distance of 1.4°, to estimate a two-dimensional (2D) model of the lithospheric magnetic anomaly field over Egypt using gradient data. The gr...

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Main Authors: Asmaa Abdellatif, Essam Ghamry, Mohamed Sobh, Adel Fathy
Format: Article
Language:English
Published: MDPI AG 2022-10-01
Series:Universe
Subjects:
Online Access:https://www.mdpi.com/2218-1997/8/10/530
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author Asmaa Abdellatif
Essam Ghamry
Mohamed Sobh
Adel Fathy
author_facet Asmaa Abdellatif
Essam Ghamry
Mohamed Sobh
Adel Fathy
author_sort Asmaa Abdellatif
collection DOAJ
description The current work makes use of the geometrical configuration of the two lower-altitude Swarm satellites (Swarm A and C), moving side by side with a longitudinal distance of 1.4°, to estimate a two-dimensional (2D) model of the lithospheric magnetic anomaly field over Egypt using gradient data. The gradient in both the north–south and the east–west directions have been inverted using the weighted damping least-squares fit technique to estimate the best model coefficients of the 2D model. The best model coefficients have been obtained under the expansion of the Legendre polynomial from degree <i>n</i> = 7 to <i>n</i> = 56. Results showed that the gradient of the field in the north–south direction is always much smoother than that in the east–west direction. The noise in the east–west direction is attributed to the different environmental conditions surrounding both satellites. The modeled field always showed smoother variations than the observed data, even for the horizontal components (<i><b>B</b><sub>x</sub></i> and <i><b>B</b><sub>y</sub></i>).
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spelling doaj.art-ab6c94aa7e8c419985cb5588a1787f7e2023-11-24T03:01:49ZengMDPI AGUniverse2218-19972022-10-0181053010.3390/universe8100530A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm MissionAsmaa Abdellatif0Essam Ghamry1Mohamed Sobh2Adel Fathy3Physics Department, Faculty of Science, Fayoum University, Fayoum 63514, EgyptNational Research Institute of Astronomy and Geophysics (NRIAG), Helwan 11421, EgyptNational Research Institute of Astronomy and Geophysics (NRIAG), Helwan 11421, EgyptPhysics Department, Faculty of Science, Fayoum University, Fayoum 63514, EgyptThe current work makes use of the geometrical configuration of the two lower-altitude Swarm satellites (Swarm A and C), moving side by side with a longitudinal distance of 1.4°, to estimate a two-dimensional (2D) model of the lithospheric magnetic anomaly field over Egypt using gradient data. The gradient in both the north–south and the east–west directions have been inverted using the weighted damping least-squares fit technique to estimate the best model coefficients of the 2D model. The best model coefficients have been obtained under the expansion of the Legendre polynomial from degree <i>n</i> = 7 to <i>n</i> = 56. Results showed that the gradient of the field in the north–south direction is always much smoother than that in the east–west direction. The noise in the east–west direction is attributed to the different environmental conditions surrounding both satellites. The modeled field always showed smoother variations than the observed data, even for the horizontal components (<i><b>B</b><sub>x</sub></i> and <i><b>B</b><sub>y</sub></i>).https://www.mdpi.com/2218-1997/8/10/530Swarm satellitesinverse theorylithospheric magnetic anomaly fieldLegendre polynomialEgypt
spellingShingle Asmaa Abdellatif
Essam Ghamry
Mohamed Sobh
Adel Fathy
A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
Universe
Swarm satellites
inverse theory
lithospheric magnetic anomaly field
Legendre polynomial
Egypt
title A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
title_full A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
title_fullStr A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
title_full_unstemmed A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
title_short A 2D Lithospheric Magnetic Anomaly Field over Egypt Using Gradient Data of Swarm Mission
title_sort 2d lithospheric magnetic anomaly field over egypt using gradient data of swarm mission
topic Swarm satellites
inverse theory
lithospheric magnetic anomaly field
Legendre polynomial
Egypt
url https://www.mdpi.com/2218-1997/8/10/530
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