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Article: The Millennium Eruption of Changbaishan Tianchi Volcano is VEI 6, not 7

TitleThe Millennium Eruption of Changbaishan Tianchi Volcano is VEI 6, not 7
Authors
KeywordsB-Tm ash
Changbaishan tianchi volcano
Isopachs
Millennium eruption
Tephra volume
VEI
Issue Date2021
Citation
Bulletin of Volcanology, 2021, v. 83, n. 11, article no. 74 How to Cite?
AbstractThe Millennium Eruption (AD 946–947) of Changbaishan Tianchi Volcano is one of the largest known eruptions in recorded history. With the help of previously published isopachs and distal ash thicknesses, we re-calculate the bulk volume of its distal eruptive product, the B-Tm ash, as 27–62 km3 and the total eruption volume as 40–98 km3. The updated volume estimates are around half of those estimated by previous studies of this seminal eruption. Our work shows that the Millennium Eruption is a VEI-6 eruption, rather than VEI-7 as previously envisaged, and its magnitude is also lower than previously thought. This has implications for regional frequency-magnitude relationships and may also partially explain the limited regional, rather than global, climatic effects of the Millennium Eruption.
Persistent Identifierhttp://hdl.handle.net/10722/324195
ISSN
2023 Impact Factor: 3.6
2023 SCImago Journal Rankings: 1.237
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorYang, Qingyuan-
dc.contributor.authorJenkins, Susanna F.-
dc.contributor.authorLerner, Geoffrey A.-
dc.contributor.authorLi, Weiran-
dc.contributor.authorSuzuki, Takehiko-
dc.contributor.authorMcLean, Danielle-
dc.contributor.authorDerkachev, A. N.-
dc.contributor.authorUtkin, I. V.-
dc.contributor.authorWei, Haiquan-
dc.contributor.authorXu, Jiandong-
dc.contributor.authorPan, Bo-
dc.date.accessioned2023-01-13T03:02:09Z-
dc.date.available2023-01-13T03:02:09Z-
dc.date.issued2021-
dc.identifier.citationBulletin of Volcanology, 2021, v. 83, n. 11, article no. 74-
dc.identifier.issn0258-8900-
dc.identifier.urihttp://hdl.handle.net/10722/324195-
dc.description.abstractThe Millennium Eruption (AD 946–947) of Changbaishan Tianchi Volcano is one of the largest known eruptions in recorded history. With the help of previously published isopachs and distal ash thicknesses, we re-calculate the bulk volume of its distal eruptive product, the B-Tm ash, as 27–62 km3 and the total eruption volume as 40–98 km3. The updated volume estimates are around half of those estimated by previous studies of this seminal eruption. Our work shows that the Millennium Eruption is a VEI-6 eruption, rather than VEI-7 as previously envisaged, and its magnitude is also lower than previously thought. This has implications for regional frequency-magnitude relationships and may also partially explain the limited regional, rather than global, climatic effects of the Millennium Eruption.-
dc.languageeng-
dc.relation.ispartofBulletin of Volcanology-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.subjectB-Tm ash-
dc.subjectChangbaishan tianchi volcano-
dc.subjectIsopachs-
dc.subjectMillennium eruption-
dc.subjectTephra volume-
dc.subjectVEI-
dc.titleThe Millennium Eruption of Changbaishan Tianchi Volcano is VEI 6, not 7-
dc.typeArticle-
dc.description.naturepublished_or_final_version-
dc.identifier.doi10.1007/s00445-021-01487-8-
dc.identifier.scopuseid_2-s2.0-85117710613-
dc.identifier.volume83-
dc.identifier.issue11-
dc.identifier.spagearticle no. 74-
dc.identifier.epagearticle no. 74-
dc.identifier.eissn1432-0819-
dc.identifier.isiWOS:000710211300001-

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