Results 61 to 70 of about 733 (165)
Abstract This comprehensive study focuses on interannual oscillations from 1 to 25 years in the F, E, and D region ionosphere. By leveraging longterm (1960–2018) continuous ground‐based ionosonde and phase height measurements in northern Germany, we have identified the peak periods and temporal variations of these oscillations using advanced analysis ...
Mani Sivakandan +5 more
wiley +1 more source
Can a 1-D mantle electrical conductivity model generate magnetic jerk differential time delays? [PDF]
Worldwide jerks occurring in 1969, 1978 and 1991 are not simultaneous at the earth's surface, showing differential delays of about 2 yr. One way to explain this intriguing temporal pattern is to consider the earth's mantle as a conductor.
Jackson, A., Pinheiro, K.
core
Abstract The Earth's inner magnetosphere contains multiple electron populations influenced by different factors. The cold electrons of the plasmasphere, warm plasma that contributes to the ring current, and the relativistic plasma of the radiation belts often seem to behave independently.
D. Rasinskaite +7 more
wiley +1 more source
The impact of geomagnetic spikes on the production rates of cosmogenic 14C and 10Be in the Earth's atmosphere [PDF]
We seek corroborative evidence of the geomagnetic spikes detected in the Near East ca. 980 BC and 890 BC in the records of the past production rates of the cosmogenic nuclides 14C and 10Be.
Alexandre Fournier +34 more
core +3 more sources
Geomagnetic and Archeomagnetic Jerks: Where Do We Stand? [PDF]
The Earth's magnetic field is generated mainly by a self‐sustaining dynamo in the fluid outer core. Known as the core or main field, the dynamo's magnetic field is not constant but changes with time, a phenomenon denoted as secular variation. Unfortunately, no common agreement exists about the definition of secular variation: While some use this term ...
Mandea, M., Olsen, N.
openaire +3 more sources
Separating DP1 and DP2 Current Pattern Contributions to Substorm‐Like Intensifications in SML
Abstract Substorms have been identified from negative bays in the AL/SML index, which traces the minimum northward ground magnetic deflection at auroral latitudes, produced by enhancements of the westward electrojet. For substorms, negative bays are caused by the closure of the Substorm Current Wedge through the ionosphere, typically localized to the ...
C. J. Lao +3 more
wiley +1 more source
Earth is a complex dynamic system and study of the geomagnetic field can provide<br />insight to the dynamic processes operative in the outer core where the main field is<br />produced by a geo-dynamo mechanism.
Baldev Arora +2 more
doaj +1 more source
Geomagnetic jerks during the Swarm era and impact on IGRF-12 [PDF]
Global geomagnetic field models can be used to study the dynamics of the core, aid satellite operation and make global digital navigation possible – from smartphones to guided drilling.
Brown, William, Macmillan, Susan
core
Assessing the importance and expression of the 6-year geomagnetic oscillation [PDF]
The first time derivative of residual length-of-day observations is known to contain a distinctive 6 year periodic oscillation. Here we theorize that through the flow accelerations at the top of the core the same periodicity should arise in the ...
Abarca del Rio +37 more
core +2 more sources
A trajectory reconstruction method based on long‐range traffic detectors is proposed, which combines Newell car‐following models, the whale optimisation algorithm and particle filters to achieve trajectory reconstruction and fusion. The experimental results show that the method can effectively improve the reconstruction accuracy.
Li Li +4 more
wiley +1 more source

