Observations of a New Foreshock Region Upstream of a Foreshock Bubble's Shock [PDF]
Earth's foreshock is a region within the solar wind upstream of Earth's bow shock filled with backstreaming solar wind particles reflected at the shock.
Vassilis Angelopoulos +2 more
exaly +3 more sources
Traveling Foreshocks and Transient Foreshock Phenomena [PDF]
AbstractWe use the multispacecraft capabilities of the Cluster and Time History of Events and Macroscale Interactions during Substorms (THEMIS) missions to show that two types of foreshock may be detected in spacecraft data. One is the global foreshock that appears upstream of the Earth's quasi‐parallel bow shock under steady or variable interplanetary
Xóchitl Blanco-Cano +2 more
exaly +4 more sources
ARTEMIS Observations of Foreshock Transients in the Midtail Foreshock
AbstractForeshock transients such as hot flow anomalies (HFAs) are frequently observed in the dayside foreshock. They can disturb the local bow shock, magnetopause, and consequently the magnetosphere‐ionosphere system through dynamic pressure perturbations. Recent multipoint observations found that such perturbations can even propagate from the dayside
Hui Zhang +2 more
exaly +2 more sources
Irregular rupture process of the 2022 Taitung, Taiwan, earthquake sequence [PDF]
In September 2022, two destructive earthquakes of moment magnitude (M w) 6.6 (foreshock) and 7.1 (mainshock) occurred in Taitung County, south-eastern Taiwan.
Yuji Yagi +3 more
doaj +2 more sources
Pervasive Foreshock Activity Across Southern California
Foreshocks have been documented as preceding less than half of all mainshock earthquakes. These observations are difficult to reconcile with laboratory earthquake experiments and theoretical models of earthquake nucleation, which both suggest that ...
Zachary E. Ross, Daniel T. Trugman
exaly +2 more sources
Relationship Between the 2019 Ridgecrest, California, MW7.1 Earthquake and Its MW6.4 Foreshock Sequence [PDF]
The 2019 Ridgecrest MW7.1 earthquake has received significant attention due to its complex fault activity. It is also noticeable for its MW6.4 foreshock sequence.
Jianchang Zheng +2 more
doaj +2 more sources
Dynamics of the Foreshock Compressional Boundary and Its Connection to Foreshock Cavities [PDF]
AbstractWe use several global hybrid (kinetic ions, fluid electrons) simulation runs for steady and time‐varying interplanetary magnetic field (IMF) conditions to examine the dynamics of the foreshock compressional boundary (FCB) and its connection to foreshock cavities.
Hui Zhang +2 more
exaly +2 more sources
Foreshock Migration Preceding the 2016 Mw 7.0 Kumamoto Earthquake, Japan
We investigated the spatiotemporal evolution of an earthquake sequence following a series of large shallow intraplate earthquakes, including a Mw 6.2 foreshock and Mw 7.0 main shock, in the Kumamoto area of Kyushu, SW Japan.
Jun'Ichi Fukuda +2 more
exaly +2 more sources
Foreshocks Explained by Cascades of Triggered Seismicity [PDF]
The observation of foreshocks preceding large earthquakes and the suggestion that foreshocks have specific properties that may be used to distinguish them from other earthquakes have raised the hope that large earthquakes may be predictable. Among proposed anomalous properties are the larger proportion than normal of large versus small foreshocks, the ...
Didier Sornette, Agnes Helmstetter
exaly +4 more sources
Helium in the Earth's foreshock: a global Vlasiator survey [PDF]
The foreshock is a region of space upstream of the Earth's bow shock extending along the interplanetary magnetic field (IMF). It is permeated by shock-reflected ions and electrons, low-frequency waves, and various plasma transients.
M. Battarbee +21 more
doaj +1 more source

