scholarly journals Regional geomagnetic field modelling: the contribution of the Istituto Nazionale di Geofisica

1997 ◽  
Vol 40 (5) ◽  
Author(s):  
A. De Santis ◽  
M. Chiappini ◽  
G. Dominici ◽  
A. Meloni

Models of the geomagnetic field are mathematical expressions able to represent the Earth's magnetic field space and time variations. Time variations on the long term basis are represented by the so-called secular variation. This paper describes and reviews recent activities of the Italian group at the Istituto Nazionale di Geofisica in regional magnetic field modelling. The models are introduced starting from the classical technique of Spherical Harmonic Analysis (SHA) undertaken for the first time by Gauss, the polynomial analysis and the regional harmonic analysis, specifically introduced as a regional analogue of SHA. In this last group the recent techniques of Spherical Cap Harmonic Analysis (SCHA), Translated Origin Spherical Cap Analysis (TOSCA) and Adjusted Spherical Cap Harmonic Analysis (ASHA) are also described and discussed.

1994 ◽  
Vol 46 (9) ◽  
pp. 789-795 ◽  
Author(s):  
Zhen-chang An ◽  
Dong-hai Tan ◽  
Yuan-fang Xu ◽  
V. P. Golovkov ◽  
N. M. Rotanova ◽  
...  

1988 ◽  
Vol 41 (3-6) ◽  
pp. 177-186 ◽  
Author(s):  
Heikki Nevanlinna ◽  
Joumi Rynö ◽  
Gerry V. Haines ◽  
Kjell Borg

Author(s):  
Maha Ali Alfheid ◽  
Mohana Faroug Attia

A spherical cap harmonic analysis (SCHA) model has been used to derive a high resolution regional model of the geomagnetic field in the southwest Pacific region over the past 400 years. Two different methods, a self-consistent and the gufm1 dipole method, have been used to fill in gaps in the available data. The data used in the analysis were largely measurements of the magnetic field recorded in ships logs on voyages of exploration in the region.  The method chosen for the investigation used a spherical cap of radius


2004 ◽  
Vol 47 (6) ◽  
pp. 1128-1134 ◽  
Author(s):  
Zuo-Wen GU ◽  
Zhen-Chang AN ◽  
Jin-Tian GUAO ◽  
Wei HAN ◽  
Zhi-Jia ZHAN

2021 ◽  
Vol 873 (1) ◽  
pp. 012030
Author(s):  
Ilham ◽  
M Syirojudin ◽  
R Margiono ◽  
A Marsono ◽  
N Ardiana

Abstract The earth’s lithospheric magnetic field is part of the main earth’s magnetic field. The lithospheric field has a very small value compared to the Earth’s main magnetic field, approximately less than 1%, and this field is generated at the earth’s crust and upper mantle. Modelling of lithospheric field is useful mainly for predicting the distribution of the value of lithospheric fields and to determine the magnetic anomaly. In this research, modelling the Earth’s lithospheric magnetic field uses Spherical Cap Harmonic Analysis (SCHA) method and this method can do modelling using regional magnetic data. The data used for the modelling are magnetic repeat station data in Indonesia region (BMKG’s Epoch) and SWARM satellite data. The results of the modelling using integrated SWARM satellite and repeat station data produce RMSE values of 64.0834 nT and the expansion of index K is 70. In addition, the results of the modelling resolution is 1.50. The value’s range of modelling’s result are -987.192 – 998.239 nT for X component, -968.189 – 949.438 nT for Y component, -981.266 – 608.676 nT for Z component, and -904.151 – 997.389 nT for total intensity are.


Sign in / Sign up

Export Citation Format

Share Document