Results 61 to 70 of about 243,128 (206)
New geomagnetic field observations in the South Atlantic Anomaly region
Three new geomagnetic observatories have been established recently around the South Atlantic geomagnetic<br />Anomaly by GeoForschungsZentrum Potsdam(GFZ), Germany, in collaboration with other institutions.
Pieter Kotzé +5 more
doaj +1 more source
OI 630 nm Airglow Observed From Space as a Diagnostic of Nighttime Low‐Latitude Ionospheric Dynamics
Abstract This study investigates the nighttime morphology of the bottomside F region (∼250 km) at low latitudes using 630 nm airglow measurements from the Visible and Infrared Spectral Imager (VISI) aboard the Ionosphere, Mesosphere, Upper Atmosphere, and Plasmasphere (IMAP) mission on the International Space Station. For this purpose, we analyzed IMAP/
Hyosub Kil +6 more
wiley +1 more source
Geomagnetic study in the area of the constructed geomagnetic observatory in Tosontsengel
This study systematically investigated how a 1-hectare site selected in Tosontsengel soum meets international standards for constructing a geomagnetic observatory. We measured the geomagnetic field exactly along the predefined profiles at the site before and after construction, produced maps showing the distribution of anomalous geomagnetic fields, and
Bayanjargal Gendenpuntsag +6 more
openaire +1 more source
Geomagnetic observatories threatened again
In its fiscal year (FY) 1988 budget, the U.S. Geological Survey (USGS) is again proposing to close two geomagnetic observatories (Eos, February 10, 1987, p. 78). Reliable sources have indicated to us that one of the contemplated closings is of an Alaskan observatory.
L. J. Lanzerotti, A. D. Chave
openaire +1 more source
The updated version of the ITalian Geomagnetic Reference Field (ITGRF) for 2000.0 and its secular variation model up to 2005.0 are presented in this paper.
J. M. Torta +5 more
doaj +1 more source
Nighttime Westward Equatorial Electrojet Observed During the January 2026 Geomagnetic Storm
Abstract The equatorial electrojet (EEJ) is a narrow band of zonal electric current flowing in the E‐region ionosphere within approximately ±2° $\pm 2{}^{\circ}$ latitude of the magnetic equator. At night, the EEJ is generally considered very weak because of low ionospheric conductivity.
Y. Yamazaki +26 more
wiley +1 more source
The recently proposed dayside current wedge likely explains the mechanism behind the well-known Carrington geomagnetic storm on 2 September 1859, as well as an event observed in Europe on 29 October 2003. Both events were swift and intense, had unusually
Eduard KOČI, Fridrich VALACH
doaj +1 more source
Secular trends in storm-level geomagnetic activity [PDF]
Analysis is made of K-index data from groups of ground-based geomagnetic observatories in Germany, Britain, and Australia, 1868.0–2009.0, solar cycles 11–23.
J. J. Love
doaj +1 more source
Abstract Reconstructing past interactions between the West Antarctic Ice Sheet (WAIS) and changing environmental conditions in the Ross Sea region can help determine long‐term WAIS stability. Existing sedimentary records reveal changes to oceanography, sea ice and ice sheet extent over the glacial‐interglacial cycles of the last ∼800 kyr.
J. W. Marschalek +26 more
wiley +1 more source
Protection against lightning at a geomagnetic observatory [PDF]
Abstract. The Sinji Vrh Geomagnetic Observatory was built on the brow of Gora, the mountain above Ajdovščina, which is a part of Trnovo plateau, and all over Europe one can hardly find an area which is more often struck by lightning than this southwestern part of Slovenia.
R. Čop +3 more
openaire +3 more sources

