Results 91 to 100 of about 295,213 (157)

Geomagnetic effects on cosmic ray propagation under different conditions for Buenos Aires and Marambio, Argentina [PDF]

open access: yes, 2014
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.
core   +1 more source

Ionospheric Response to the May 11, 2024, Geomagnetic Superstorm over Ecuador [PDF]

open access: yesarXiv
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]

open access: yes, 2018
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
core   +1 more source

No Major Solar Flares but the Largest Geomagnetic Storm in the Present Solar Cycle

open access: yes, 2015
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
semanticscholar   +1 more source

Intense Geomagnetic Storms during Solar Cycles 23-25 [PDF]

open access: yesarXiv
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]

open access: yes
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
core   +1 more source

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