Results 111 to 120 of about 1,592 (224)
Anomalous Secular Variation of Geomagnetic Total Intensity In Chugoku District, Japan [PDF]
, 1972 In 1971 Geomagnetic surveys in the Chugoku district have been carried out by using a portable proton precession magnetometer. The ordinary method of epoch reduction to eliminate non-local changes in the geomagnetic field has been slightly modified by ...
SUMITOMO, Norihiko
core
Annals of Geophysics, 2002 The Earth's magnetic field varies over a wide range of characteristic times, say, from years to centuries, and more. In order to detect some nonlinear features of the geomagnetic field evolution we first apply a nonlinear spectral technique, i.e ...
A. De Santis, R. Tozzi
doaj +1 more source
Journal of Geophysical Research: Space Physics, Volume 131, Issue 6, June 2026.Abstract The substorm current wedge constitutes the backbone of the substorm current system. Its field‐aligned current components include an upward current in the premidnight sector and a downward current in the midnight‐morning sector, which connect the auroral ionosphere to the magnetotail.
Tsugunobu Nagai, Iku Shinohara
wiley +1 more source
Space Weather, Volume 24, Issue 6, June 2026.Abstract The geomagnetic storm on 1 June 2025 generated pronounced large‐scale traveling ionospheric disturbances (LSTIDs) over China, captured by dense GNSS networks. It has been unclear whether network real‐time kinematic (NRTK) positioning, which relies on spatial interpolation from multiple reference stations, remains effective under such extreme ...
Tong Liu +8 more
wiley +1 more source
The First Archaeomagnetic Age at Tiwanaku and Implications for Dating Andean Metallurgical Furnaces
Archaeometry, Volume 68, Issue 3, Page 317-329, June 2026.ABSTRACT This paper presents the first archaeomagnetic dating at Tiwanaku (Andean Altiplano). We compared the geomagnetic field values recorded by a metallurgical furnace against an updated SHAWQ2k‐SH global model and a regional intensity curve, both of which include, for the first time, high‐quality intensity data from the Southern Hemisphere. Results
Judit del Río +6 more
wiley +1 more source
Report on the magnetic survey in Slovakia for the 2014.5 epoch
Contributions to Geophysics and Geodesy, 2016 The models of the distribution of the elements of the geomagnetic field must be updated regularly. For this purpose geomagnetic measurements have to be carried out repeatedly at geomagnetic observatories as well as at temporary observation points.
Fridrich VALACH +3 more
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Simple additional constraints on regional models of the geomagnetic secular variation field
, 1996 Lecter section of Physics of the Earth and Planetary Interiors 97 (1996)Standard ways of building regional models of the geomagnetic field fail when one wishes to model secular variation (SV).
Torta, J. M., De Santis, A., Falcone, C.
core
How does Chinese loess become magnetized?
, 2010 EThOS - Electronic Theses Online ServiceGBUnited ...
Zhao, Xiang
core
Bottom-up control of geomagnetic secular variation by the Earth's inner core
, 2013 Temporal changes in the Earth’s magnetic field, known as geomagnetic secular variation, occur most prominently at low latitudes in the Atlantic hemisphere1, 2 (that is, from −90 degrees east to 90 degrees east), whereas in the Pacific hemisphere there is
Finlay, Chris +6 more
core +1 more source
, 2020 A marine sediment core from the western Mediterranean provides a new high-resolution 4500 year record of palaeomagnetic secular variation and relative palaeointensity.
Florindo F. +13 more
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