How large-scale water cycles influence earthquakes in California

A new study shows how seasonal changes in large-scale water cycles in California influence small-scale quake activity. It confirms that the annual hydrological loading cycle modulates microseismicity in California. The results of the study reveal how snow, rain, snowmelt and runoff — as well as water changes related to agriculture — alter stress on regional faults, with seismic consequence, in some cases.

Stress changes on or near fault lines can drive seismic activity. Such changes may be caused by myriad phenomena, including variations in fluid pore pressure. Here, Christopher Johnson and colleagues wanted to further explore a role for alternating wet and dry cycles in altering ground stress, and ultimately, in driving tremors. They compared seasonal changes in ground stress estimated from GPS data from 2006 to 2014 to California earthquake rates between these years, finding that slight changes in stress to the ground associated with water and snow accumulation, snow melt, runoff, or irrigation for agriculture did influence earthquake likelihood. In the San Andreas fault system, for example, conditions for quakes were more favorable for faulting during the dryer summer months, the authors say. Northern California faults in the UCERF3 fault model shown with the annual peak-to-peak Coulomb […]

Full article: How large-scale water cycles influence quake activity in California

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