Geomagnetic effects on cosmic ray propagation under different conditions for Buenos Aires and Marambio, Argentina [PDF]
The geomagnetic field (Bgeo) sets a lower cutoff rigidity (Rc) to the entry of cosmic particles to Earth which depends on the geomagnetic activity. From numerical simulations of the trajectory of a proton using different models for Bgeo (performed with ...
Dasso, Sergio, Masías-Meza, Jimmy J.
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Geomagnetic Storms and the Space Around the Earth [PDF]
Sydney Chapman
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Ionospheric Response to the May 11, 2024, Geomagnetic Superstorm over Ecuador [PDF]
This study investigates the impact of the G5 geomagnetic storm on Total Electron Content (TEC) derived from the Global Positioning System (GPS) in Gal\'apagos, Ecuador (geographic latitude 0.1807{\deg} S, longitude 78.4678{\deg} W) during May 10-13, 2024. Using vertical TEC (VTEC) data from a single pseudorandom noise (PRN) code, along with the average
arxiv
Observations of Ion Density and Temperature around the International Space Station During two Geomagnetic Storms [PDF]
The International Space Station (ISS) is a low Earth orbit research facility and host to an international crew. Geomagnetic storms cause changes in the Earth’s magnetic field and affect the ion density and temperature in the ionosphere which could pose a
Wright, Alex M
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No Major Solar Flares but the Largest Geomagnetic Storm in the Present Solar Cycle
A severe geomagnetic storm, and the largest in solar cycle 24, occurred on 17–18 March 2015 without significant precursor Xor M-type solar flares.
Y. Kamide, K. Kusano
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Statistics of Geomagnetic Storms and Solar Activity [PDF]
Þorsteinn Sæmundsson
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Explorer 12 observations of the temporal variations of low-energy electron intensities in the outer radiation zone during geomagnetic storms [PDF]
L. A. Frank
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Intense Geomagnetic Storms during Solar Cycles 23-25 [PDF]
Intense geomagnetic storms are characterized by a minimum value of the Dst index at or below -100 nT. It is well known that these storms are caused by the southward magnetic fields in coronal mass ejections (CMEs) and corotating interaction regions (CIRs). While CIR storms are confined to Dst values at or above -150 nT, CME storms can reach Dst -500 nT
arxiv
Thermospheric Heating and Cooling Times During Geomagnetic Storms, Including Extreme Events [PDF]
We present the first quantitative calculations of thermospheric heating and cooling times for geomagnetic storms of different intensity, including extreme events.
Oliveira, Denny M., Zesta, Eftyhia
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Corrigenda [to “Scintillation counter observations of auroral X rays during the geomagnetic storm of May 12, 1959” by P. D. Bhavsar] [PDF]
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