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                              <gco:CharacterString>INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology</gco:CharacterString>
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                              <gco:CharacterString>Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services</gco:CharacterString>
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                  <gco:CharacterString>Pyroclastic Density Currents (PDCs) are among the most hazardous geological phenomena, posing challenges for predicting their impacts during eruptions. PDCs are complex, multiphase flows where density stratification significantly influences mixing, deposition, and runout. Simplified models like box models and depth-averaged approaches often assume vertically well-mixed currents, but the impact of these assumptions on mobility has been a focus of recent studies. To explore the effects of density stratification and buoyancy reversal on PDC behavior, we conducted 3D multiphase flow simulations based on heated particle-laden saline water experiments. Results showed distinct behavior for buoyant and non-buoyant currents: buoyant currents exhibited a unique density profile with a minimum at the nose, while non-buoyant currents followed typical Rousean stratification. These differences arise from interactions between density stratification and thermal buoyancy, which affect flow runout. Our findings reveal that fluid buoyancy slows particle settling, enhances vertical mixing, and limits spanwise spreading, aligning with experimental observations. However, the bulk Richardson number fails to accurately describe entrainment in these flows, suggesting a need to refine parameterization in depth-averaged models to better capture the transient nature of PDCs and improve hazard predictions.</gco:CharacterString>
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