FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3019331211> ?p ?o ?g. }

• W3019331211 endingPage "116268" @default.
• W3019331211 startingPage "116268" @default.
• W3019331211 abstract "After several months of eruptive activity, the subaerial cone of Anak Krakatau collapsed on December 22, 2018. The landslide event generated a tsunami that had deadly consequences within the Sunda Strait in Indonesia. Such significant collapse events are common in the geologic record but are a rare phenomenon, in the instrumented record. However, these events can have a potentially large impact on society. We have reconstructed the collapse, along with the activity preceding and following it, by combining information from official reports, remote geophysical observations, and local eyewitness accounts. It appears that the collapse of Anak Krakatau's subaerial cone led to a drastic change in the eruptive style from continuous Strombolian explosions to sustained Surtseyan. Those changes are detectable in the seismo-acoustic measurements, which, when combined with eyewitnesses, allows us to reconstruct the timing and phenomenology of the sequence. Our analysis reveals that intense eruptive activity generated sustained infrasound, unusual but not unique at Anak Krakatau, starting approximately eight hours before the collapse. Within this timeframe, two seismic signals consistent with minor mass movements as well as a momentary quiescence were identified prior to the main collapse. The data presented here indicate that Anak Krakatau failed in one collapse event, producing a tsunami with multiple waves around the volcano, the last one being the largest. Following the collapse, three volcanic plumes could be clearly identified in the satellite data and by eyewitnesses, as well as spectral lines in the seismic data. These lines, observed up to 371 km, suggest a repeating energetic explosive source lasting for seven days. The collapse produced multiple infrasound arrivals observed at regional infrasound stations, but was not recorded on the regional hydroacoustic network. Our analysis of the eruptive sequence demonstrates that a detailed eruption chronology can be reconstructed using remote methods, even in the event of failure or destruction of local monitoring infrastructure. This event also highlights that tsunamigenic flank collapses can occur with little to no warning, and be difficult to interpret in real-time, as a significant amount of non-operational analysis was required after the event, to complete the chronology." @default.
• W3019331211 created "2020-05-01" @default.
• W3019331211 creator A5004220644 @default.
• W3019331211 creator A5010169619 @default.
• W3019331211 creator A5014768448 @default.
• W3019331211 creator A5019883972 @default.
• W3019331211 creator A5029315818 @default.
• W3019331211 creator A5039700734 @default.
• W3019331211 creator A5043575239 @default.
• W3019331211 creator A5056520287 @default.
• W3019331211 creator A5065779231 @default.
• W3019331211 creator A5067307053 @default.
• W3019331211 creator A5071755272 @default.
• W3019331211 creator A5081150053 @default.
• W3019331211 creator A5085471056 @default.
• W3019331211 date "2020-07-01" @default.
• W3019331211 modified "2023-10-09" @default.
• W3019331211 title "Reconstruction of the 2018 tsunamigenic flank collapse and eruptive activity at Anak Krakatau based on eyewitness reports, seismo-acoustic and satellite observations" @default.
• W3019331211 cites W1508782536 @default.
• W3019331211 cites W1845703535 @default.
• W3019331211 cites W1910038890 @default.
• W3019331211 cites W1912141177 @default.
• W3019331211 cites W1966835625 @default.
• W3019331211 cites W1975934908 @default.
• W3019331211 cites W1978544644 @default.
• W3019331211 cites W2024594795 @default.
• W3019331211 cites W2028244599 @default.
• W3019331211 cites W2076217858 @default.
• W3019331211 cites W2082435776 @default.
• W3019331211 cites W2091887506 @default.
• W3019331211 cites W2101459764 @default.
• W3019331211 cites W2101870731 @default.
• W3019331211 cites W2144542233 @default.
• W3019331211 cites W2158752141 @default.
• W3019331211 cites W2329873546 @default.
• W3019331211 cites W2345254164 @default.
• W3019331211 cites W2464420131 @default.
• W3019331211 cites W2607626078 @default.
• W3019331211 cites W2626880330 @default.
• W3019331211 cites W2783451551 @default.
• W3019331211 cites W2787838759 @default.
• W3019331211 cites W2891165789 @default.
• W3019331211 cites W2891963964 @default.
• W3019331211 cites W2912862599 @default.
• W3019331211 cites W2942660299 @default.
• W3019331211 cites W2961157827 @default.
• W3019331211 cites W2966200833 @default.
• W3019331211 cites W2968460136 @default.
• W3019331211 cites W2970879027 @default.
• W3019331211 cites W2977341578 @default.
• W3019331211 cites W2979711398 @default.
• W3019331211 cites W2979860435 @default.
• W3019331211 cites W2998749755 @default.
• W3019331211 cites W3003809830 @default.
• W3019331211 cites W3009931749 @default.
• W3019331211 doi "https://doi.org/10.1016/j.epsl.2020.116268" @default.
• W3019331211 hasPublicationYear "2020" @default.
• W3019331211 type Work @default.
• W3019331211 sameAs 3019331211 @default.
• W3019331211 citedByCount "20" @default.
• W3019331211 countsByYear W30193312112020 @default.
• W3019331211 countsByYear W30193312112021 @default.
• W3019331211 countsByYear W30193312112022 @default.
• W3019331211 countsByYear W30193312112023 @default.
• W3019331211 crossrefType "journal-article" @default.
• W3019331211 hasAuthorship W3019331211A5004220644 @default.
• W3019331211 hasAuthorship W3019331211A5010169619 @default.
• W3019331211 hasAuthorship W3019331211A5014768448 @default.
• W3019331211 hasAuthorship W3019331211A5019883972 @default.
• W3019331211 hasAuthorship W3019331211A5029315818 @default.
• W3019331211 hasAuthorship W3019331211A5039700734 @default.
• W3019331211 hasAuthorship W3019331211A5043575239 @default.
• W3019331211 hasAuthorship W3019331211A5056520287 @default.
• W3019331211 hasAuthorship W3019331211A5065779231 @default.
• W3019331211 hasAuthorship W3019331211A5067307053 @default.
• W3019331211 hasAuthorship W3019331211A5071755272 @default.
• W3019331211 hasAuthorship W3019331211A5081150053 @default.
• W3019331211 hasAuthorship W3019331211A5085471056 @default.
• W3019331211 hasBestOaLocation W30193312111 @default.
• W3019331211 hasConcept C113754120 @default.
• W3019331211 hasConcept C120806208 @default.
• W3019331211 hasConcept C127313418 @default.
• W3019331211 hasConcept C165205528 @default.
• W3019331211 hasConcept C186295008 @default.
• W3019331211 hasConcept C193229666 @default.
• W3019331211 hasConcept C8058405 @default.
• W3019331211 hasConcept C84983702 @default.
• W3019331211 hasConceptScore W3019331211C113754120 @default.
• W3019331211 hasConceptScore W3019331211C120806208 @default.
• W3019331211 hasConceptScore W3019331211C127313418 @default.
• W3019331211 hasConceptScore W3019331211C165205528 @default.
• W3019331211 hasConceptScore W3019331211C186295008 @default.
• W3019331211 hasConceptScore W3019331211C193229666 @default.
• W3019331211 hasConceptScore W3019331211C8058405 @default.
• W3019331211 hasConceptScore W3019331211C84983702 @default.
• W3019331211 hasFunder F4320320709 @default.
• W3019331211 hasFunder F4320320751 @default.
• W3019331211 hasLocation W30193312111 @default.

• next