Research news on p wave

In geophysics, a P wave (primary wave) is a type of body seismic wave characterized by longitudinal particle motion parallel to the direction of propagation, making it the fastest seismic phase traveling through the Earth. It involves alternating compressions and rarefactions of the medium and can propagate through solids, liquids, and gases, with velocity controlled by the medium’s elastic moduli (bulk and shear) and density. P waves are crucial for seismic tomography, Earth structure studies, and earthquake source characterization, as their arrival times and amplitude patterns constrain subsurface velocity distributions and discontinuities such as the Mohorovičić discontinuity and core–mantle boundary.

In seconds, fiber optic cables detect earthquake size

Scientists have discovered a new way to determine how big an earthquake may become just seconds after it begins. In a new study published in Nature Communications, researchers from the U.S. Geological Survey (USGS) and Cal ...

Seismic attenuation techniques reveal what lies beneath Taiwan

As seismic waves travel through Earth, they gradually lose energy, a process called attenuation. That energy loss doesn't happen uniformly—some features in the crust sap far more energy from seismic waves than others. Researchers ...