A buoyancy-driven flow model with phase change and asymmetric geometry reproduces uplift variations and localized flow at Campi Flegrei, predicting nonlinear acceleration and shallow seismicity.
Earthquake Rupture Velocity and Stress Drop Interaction in the Campi Flegrei V olcanic Caldera
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Toward buoyancy-driven flow at Campi Flegrei: coupled phase change and asymmetric geometry
A buoyancy-driven flow model with phase change and asymmetric geometry reproduces uplift variations and localized flow at Campi Flegrei, predicting nonlinear acceleration and shallow seismicity.