{"id":153,"date":"2025-10-12T07:56:51","date_gmt":"2025-10-12T07:56:51","guid":{"rendered":"https:\/\/thm.iavceivolcano.org\/?page_id=153"},"modified":"2025-11-24T16:03:58","modified_gmt":"2025-11-24T16:03:58","slug":"volcanic-plume-benchmarking-working-group","status":"publish","type":"page","link":"https:\/\/thm.iavceivolcano.org\/volcanic-plume-benchmarking-working-group\/","title":{"rendered":"Volcanic Plume Benchmarking working group"},"content":{"rendered":"\n<p>The Volcanic Plume Benchmarking (VPB) working group aims to improve the fundamental<br>understanding of volcanic plume dynamics and, ultimately, to improve the ability to forecast<br>the dispersion of volcanic ash during eruptive crises. Explosive volcanic plumes can produce<br>laterally spreading ash clouds or pyroclastic density currents, each of which presents<br>particular societal and environmental impacts. These are dangerous and devastating<br>phenomena, and, understandably, in situ data are rare to nonexistent. Volcanologists have<br>hence developed several strategies for the indirect study of eruption plumes: i) scaled<br>analogue experimental models using either water-particle or air-particle mixtures to<br>simulate the plume; ii) field observations, including the analysis of eruption products and<br>their spatial distributions, and satellite and remote sensing of the plumes; iii) numerical<br>modelling either through transient simulations where the full three-dimensional (3D) motion<br>of the plume is modelled or through steady-state one-dimensional (1D) models where<br>several aspects of the plume motion are parameterised. Whilst numerous numerical models<br>have been proposed to simulate volcanic plumes, there is currently relatively little<br>agreement between their predictions. The VPB working group was formed to address these<br>shortcomings through the establishment of a set of benchmarked analogue models and<br>standardised experimental protocols, and a set of detailed field observations. These data<br>sets will then be used to test, validate and calibrate current numerical models and to ease<br>the development of new models. The VPB working group will meet regularly to discuss the<br>latest results and hold \u201chackathon\u201d-style sessions for the acquisition of new data. Our goals<br>are closely aligned with several of the THM Commission\u2019s goals, and, indeed, several<br>members are already involved in the Commission or in its various working groups. Thus, we<br>ask to be considered as a recognised working group within the THM Commission.<\/p>\n\n\n\n<p><\/p>\n\n\n\n<figure class=\"block-image size-large is-resized\"><div class=\"loading-placeholder shine\" style=\"aspect-ratio: 1\/ 0.556358381503\"><img decoding=\"async\" data-sizes=\"(max-width: 692px) 100vw, 692px\" data-src=\"https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop.jpg\" data-srcset=\"https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop.jpg 2200w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-300x167.jpg 300w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-1024x570.jpg 1024w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-768x427.jpg 768w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-1536x855.jpg 1536w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-2048x1139.jpg 2048w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-252x140.jpg 252w\" width=\"692\" height=\"385\" src=\"\/\/:0\" class=\"lazyload\" alt=\"Img 0267 Crop\" style=\"width:692px;height:auto\"   loading=\"lazy\" \/><noscript><img decoding=\"async\" width=\"692\" height=\"385\" src=\"https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop.jpg\" class=\"lazyload\" alt=\"Img 0267 Crop\" style=\"width:692px;height:auto\" srcset=\"https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop.jpg 2200w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-300x167.jpg 300w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-1024x570.jpg 1024w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-768x427.jpg 768w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-1536x855.jpg 1536w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-2048x1139.jpg 2048w, https:\/\/thm.iavceivolcano.org\/content\/uploads\/sites\/13\/2025\/11\/img_0267_crop-252x140.jpg 252w\" sizes=\"auto, (max-width: 692px) 100vw, 692px\" loading=\"lazy\" \/><\/noscript><\/div><\/figure>\n\n\n\n<p><br><em><strong>Current working group members and collaborators:<\/strong><\/em><br>David Jessop (LMV, France; david.jessop@uca.fr)<br>Thomas Aubry (U. Oxford, UK; thom.aubry@gmail.com)<br>Guillaume Carazzo (Institut de Physique du Globe de Paris, France; carazzo@ipgp.fr)<br>Valentin Freret Lorgeril (LMV, France; Valentin.FRERET_LORGERIL@uca.fr)<br>Franck Donnadieu (LMV, France; franck.donnadieu@uca.fr)<br>Julia Eychenne (LMV, France; julia.eychenne@uca.fr)<br>Audrey Michaud-Dubuy (LMV, France; Audrey.MICHAUD-DUBUY@uca.fr)<br>Matteo Cerminara (INGV Pisa, Italy; matteo.cerminara@ingv.it)<br>Ulrich K\u00fcppers (Ludwig-Maximilians-Universit\u00e4t M\u00fcnchen, Germany; u.kueppers@lmu.de)<br>Johan Gilchrist (U. Oregon, USA; jgilchr2@uoregon.edu)<br>Josef Dufek (U. Oregon, USA; jdufek@uoregon.edu)<br>Thomas Giachetti (U. Oregon, USA; tgiachet@uoregon.edu)<br>Eric Breard (U. Edinburgh, UK; eric.breard@ed.ac.uk)<br>Yujiro Suzuki (U. Tokyo, Japan; yujiro@eri.u-tokyo.ac.jp)<br>Samantha Engwell (British Geological Survey, UK; sameng@bgs.ac.uk)<br>LMV = Laboratoire Magmas et Volcans<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The Volcanic Plume Benchmarking (VPB) working group aims to improve the fundamentalunderstanding of volcanic plume dynamics and, ultimately, to improve the ability to forecastthe dispersion of volcanic ash during eruptive crises. Explosive volcanic plumes can producelaterally spreading ash clouds or&#8230;<\/p>\n","protected":false},"author":400,"featured_media":0,"parent":0,"menu_order":8,"ping_status":"closed","template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","footnotes":""},"class_list":["post-153","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/pages\/153","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/users\/400"}],"version-history":[{"count":2,"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/pages\/153\/revisions"}],"predecessor-version":[{"id":159,"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/pages\/153\/revisions\/159"}],"wp:attachment":[{"href":"https:\/\/thm.iavceivolcano.org\/api\/wp\/v2\/media?parent=153"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}