Campi Flegrei (CF) is an example of an active caldera containing densely populated settlements at very high risk of pyroclastic density currents (PDCs). We present here an innovative method for assessing background spatial PDC hazard in a caldera setting with probabilistic invasion maps conditional on the occurrence of an explosive event. The method encompasses the probabilistic assessment of potential vent opening positions, derived in the companion paper, combined with inferences about the spatial density distribution of PDC invasion areas from a simplified flow model, informed by reconstruction of deposits from eruptions in the last 15 ka. The flow model describes the PDC kinematics and accounts for main effects of topography on flow pro...
The Campi Flegrei caldera is a complex and resurgent structure, and its active portion has been the ...
Pyroclastic density currents (PDCs) are hot flowing mixtures of gas and pyroclasts that can cause wi...
This study presents a new method for producing long-term hazard maps for pyroclastic density curren...
Campi Flegrei (CF) is an example of an active caldera containing densely populated settlements at ve...
Campi Flegrei (CF) is an example of an active caldera containing densely populated settlements at ve...
This study presents a new method for producing long-term hazard maps for pyroclastic density current...
Campi Flegrei is an active volcanic area situated in the Campanian Plain (Italy) and dominated by a ...
This study presents a new method for producing long-term hazard maps for pyroclastic density curren...
The Campi Flegrei caldera is a restless structure affected by general subsidence and ongoing resurge...
The Campi Flegrei volcanic field (Italy) poses very high risk to the highly urbanized Neapolitan are...
The metropolitan area of Napoli (∼3 M inhabitants) in southern Italy is located in between two explo...
<div><p>The Campi Flegrei volcanic field (Italy) poses very high risk to the highly urbanized Neapol...
The Campi Flegrei caldera is a complex and resurgent structure, and its active portion has been the ...
Pyroclastic density currents (PDCs) are hot flowing mixtures of gas and pyroclasts that can cause wi...
This study presents a new method for producing long-term hazard maps for pyroclastic density curren...
Campi Flegrei (CF) is an example of an active caldera containing densely populated settlements at ve...
Campi Flegrei (CF) is an example of an active caldera containing densely populated settlements at ve...
This study presents a new method for producing long-term hazard maps for pyroclastic density current...
Campi Flegrei is an active volcanic area situated in the Campanian Plain (Italy) and dominated by a ...
This study presents a new method for producing long-term hazard maps for pyroclastic density curren...
The Campi Flegrei caldera is a restless structure affected by general subsidence and ongoing resurge...
The Campi Flegrei volcanic field (Italy) poses very high risk to the highly urbanized Neapolitan are...
The metropolitan area of Napoli (∼3 M inhabitants) in southern Italy is located in between two explo...
<div><p>The Campi Flegrei volcanic field (Italy) poses very high risk to the highly urbanized Neapol...
The Campi Flegrei caldera is a complex and resurgent structure, and its active portion has been the ...
Pyroclastic density currents (PDCs) are hot flowing mixtures of gas and pyroclasts that can cause wi...
This study presents a new method for producing long-term hazard maps for pyroclastic density curren...