排序方式： 共有13条查询结果，搜索用时 78 毫秒
11.
The Earth's crust is magnetized down to the Curie-temperature depth at about 10 to 50 km. This limited depth extent of the crustal magnetization is discernible in the power spectra of magnetic maps of South Africa and Central Asia. At short wavelengths, the power increases as rapidly towards longer wavelengths as expected for a self-similar magnetized crust with unlimited depth extent. Above wavelengths of about 100 km the power starts increasing less rapidly, indicating the absence of deep-seated sources. To quantify this effect we derive the theoretical power spectrum due to a slab carved out of a self-similar magnetization distribution. This model power spectrum matches the power spectra of South Africa and Central Asia for a self-similarity parameter of β = 4 and Curie temperature depths of 15 to 20 km. 相似文献
12.
The 9th-Generation International Geomagnetic Reference Field 总被引：5，自引：0，他引：5
International Association of Geomagnetism Aeronomy Division V Working Group Participating members: S. Macmillan S. Maus T. Bondar A. Chambodut V. Golovkov R. Holme B. Langlais V. Lesur F. Lowes H. Lühr W. Mai M. Mandea N. Olsen M. Rother T. Sabaka A. Thomson I. Wardinski 《Geophysical Journal International》2003,155(3):1051-1056
13.
The geomagnetic power spectrum 总被引：1，自引：0，他引：1
Stefan Maus 《Geophysical Journal International》2008,174(1):135-142
Combining CHAMP satellite magnetic measurements with aeromagnetic and marine magnetic data, the global geomagnetic field has now been modelled to spherical harmonic degree 720. An important tool in field modelling is the geomagnetic power spectrum. It allows the comparison of field models estimated from different data sets and can be used to identify noise levels and systematic errors. A correctly defined geomagnetic power spectrum is flat (white) for an uncorrelated field, such as the Earth's crustal magnetic field at long wavelengths. It can be inferred from global spherical harmonic models as well as from regional grids. Marine and aeromagnetic grids usually represent the anomaly of the total intensity of the magnetic field. Appropriate corrections have to be applied in estimating the geomagnetic power spectrum from such data. The comparison of global and regional spectra using a consistently defined azimuthally averaged geomagnetic power spectrum facilitates quality control in field modelling and should provide new insights in magnetic anomaly interpretation. 相似文献