In this study, we demonstrate an approach for inverting earthquake source parameters based on high-rate global positioning system (GPS) velocity seismograms. The velocity records obtained from single-station GPS velocity solutions with broadcast ephemeris are used directly for earthquake source parameter inversion using the Cut and Paste method, without requiring conversion of the velocity records into displacement records. Taking the El Mayor-Cucapah earthquake as an example, GPS velocity records from 10 stations with reasonable azimuthal coverage provide earthquake source parameters very close to those from the Global centroid moment tensor (Global CMT) solution. In sparse network tests, robust source parameters with acceptable bias can be achieved with as few as three stations. When the number of stations is reduced to two, the bias in rake angle becomes appreciable, but the magnitude and strike estimations are still robust. The results of this study demonstrate that rapid and reliable estimation of earthquake source parameters can be obtained from GPS velocity data. These parameters could be used for early earthquake warning and shake map construction, because such GPS velocity records can be obtained in real time.
high-rate GPS velometer, GPS velocity determination, CAP method, earthquake source parameters, sparse networkThe global positioning system (GPS) was designed to be a positioning, navigation, and timing (PNT) system. Currently, however, the system is used for applications far beyond its original intended design (Misra and Enge, 2006; HofmannWellenhof et al., 2008). In earthquake research, dynamic GPS displacement records with a 1 Hz or higher sampling rate, known as high-rate GPS, are now widely used to capture earthquake dynamic waveforms and to invert earthquake source parameters and rupture processes independently or together with seismological data (Larson et al.-rate GPS is not as sensitive as traditional instruments, e.g., velocity-type broadband seismometers and accelerometer-type strong motion instruments, high-rate GPS has become more popular in the last two decades. Compared with the traditional seismological instruments, this method avoids the problems of record clipping, tilting, and long-period drift that result from integrating acceleration or velocity into displacements. High-rate GPS can directly obtain arbitrarily large dynamic displacements (waveforms) and static offsets of earthquakes (co-seismic deformation) with millimeter-to centimeter-scale accuracy in the post-processing mode; in contrast, real-time and near real-time processing approaches have lower accuracy (Bock et al., 2004;Larson et al., 2007;