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Foreshock Transients and Their Geoeffects
2020<p>Foreshock transients are frequently observed upstream from the bow shock (such as Hot Flow&#160;Anomalies, foreshock cavities, and foreshock bubbles). They play a significant role in the mass, energy&#160;and momentum transport from the solar wind into the magnetosphere and impact the whole&#160 ...
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Foreshock fluctuation and its behaviors
The foreshock region is a turbulent area that forms before a quasi-parallel shock. It is caused by the interaction between reflected particles from the bow shock and oncoming waves in the solar wind. Typically, the foreshock is located on the dawn side.Gilbert Pi +2 more
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Spatio-temporal foreshock evolution of the 2019 M 6.4 and M 7.1 Ridgecrest, California earthquakes
Earth and Planetary Science Letters, 2020Hui Huang, Lingsen Meng, Roland Burgmann
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A Foreshock Bubble Driven by an IMF Tangential Discontinuity: 3D Global Hybrid Simulation
Geophysical Research Letters, 2021Chih-Ping Wang, Xueyi Wang, Yu Lin
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Foreshock sequences and short-term earthquake predictability on East Pacific Rise transform faults
Nature, 2005Jeffrey J Mcguire +2 more
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THEMIS observations of tangential discontinuity‐driven foreshock bubbles
Geophysical Research Letters, 2015Terry Liu +2 more
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Foreshock bubbles and their global magnetospheric impacts
Journal of Geophysical Research, 2010Nick Omidi +2 more
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