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.
Tracking the 2007–2023 Magma-Driven Unrest at Campi Flegrei Caldera (Italy)
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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.