Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Wim Degruyter"'
Autor:
Eveanjelene Snee, Paul Antony Jarvis, Riccardo Simionato, Simona Scollo, Michele Prestifilippo, Wim Degruyter, Costanza Bonadonna
Publikováno v:
Volcanica, Vol 6, Iss 2, Pp 447-458 (2023)
Video cameras provide vital information on volcanic plumes from explosive eruptions, such as plume height, for monitoring and research. These images must be calibrated to get accurate quantitative data. However, the presence of wind complicates any c
Externí odkaz:
https://doaj.org/article/a515e7f9844144c48c602f269117d68a
Autor:
Valentin Freret-Lorgeril, Wim Degruyter, Simona Scollo, Costanza Bonadonna, Eduardo Rossi, Evie Snee
Publikováno v:
Journal of geophysical research, Vol. 126, No 12 (2021) P. e2020JB021360
Explosive basaltic eruptions pose significant threats to local communities, regional infrastructures and international airspace. They produce tephra plumes that are often associated with a lava fountain, complicating their dynamics. Consequently, sou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8cae806484f43e30c5afcb594e89f7ea
Publikováno v:
Nature Geoscience, 12 (9)
Storage pressures of magma chambers influence the style, frequency and magnitude of volcanic eruptions. Neutral buoyancy or rheological transitions are commonly assumed to control where magmas accumulate and form such chambers. However, the density o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06f5c48bc2b3652619820981ba3a049c
https://doi.org/10.1038/s41561-019-0415-6
https://doi.org/10.1038/s41561-019-0415-6
Autor:
Konstantinos Kyriakopoulos, Olivier Bachmann, Peter Tollan, Wim Degruyter, Ben S. Ellis, Răzvan-Gabriel Popa
Publikováno v:
Journal of Volcanology and Geothermal Research, 387 . Art.Nr. 106666.
Highlights • In water-rich silicic systems effusions can be generated by magmas with higher water contents than explosions. • The paper presents the comparative example of effusive and explosive deposits erupted at Nisyros-Yali. • Explosive eru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::300671e3612eb19f5b1d5dd51a83d452
https://orca.cardiff.ac.uk/id/eprint/125517/1/Popa_etal_2019_JVGR_postprint.pdf
https://orca.cardiff.ac.uk/id/eprint/125517/1/Popa_etal_2019_JVGR_postprint.pdf
Publikováno v:
Geochemistry, Geophysics, Geosystems, 18 (11)
Geochemistry, Geophysics, Geosystems, 18 (11)
ISSN:1525-2027
ISSN:1525-2027
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fb8a3e56c57e5af13cccd2a9896d4b55
https://doi.org/10.1002/2017gc007219
https://doi.org/10.1002/2017gc007219
Publikováno v:
Geochemistry, Geophysics, Geosystems, 18 (8)
Magma degassing fundamentally controls the Earth's volatile cycles. The large amount of gas expelled into the atmosphere during volcanic eruptions (i.e. volcanic outgassing) is the most obvious display of magmatic volatile release. However, owing to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1ccfb02d4153b5cbb611f6fe833670e
https://doi.org/10.1002/2017gc006912
https://doi.org/10.1002/2017gc006912
Publikováno v:
Geochemistry, Geophysics, Geosystems, 20 (3)
Crustal magma chambers can grow to be hundreds to thousands of cubic kilometers, potentially feeding catastrophic caldera‐forming eruptions. Smaller‐volume chambers are expected to erupt frequently and freeze quickly; a major outstanding question
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::16fb2b24da244b3a4487865584244f2d
https://hdl.handle.net/20.500.11850/340413
https://hdl.handle.net/20.500.11850/340413
Publikováno v:
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 377 (2139)
Only a small fraction (approx. 1–20%) of magmas generated in the mantle erupt at the surface. While volcanic eruptions are typically considered as the main exhaust pipes for volatile elements to escape into the atmosphere, the contribution of magma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::488373d0d0a992f9201ee05951351643
https://hdl.handle.net/20.500.11850/344711
https://hdl.handle.net/20.500.11850/344711
Publikováno v:
Earth and Planetary Science Letters, Vol. 505 (2019) pp. 1-12
Plume height is an important parameter routinely used to characterize and classify explosive eruptions. Though the strategies to estimate key eruption source parameters such as erupted volume and mass flow rate have evolved over the past few decades,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fb7257075af464831e016b5d6c6f6481
https://orca.cardiff.ac.uk/id/eprint/115842/1/WD_Rossi_etal_2018_EPSL_postprint.pdf
https://orca.cardiff.ac.uk/id/eprint/115842/1/WD_Rossi_etal_2018_EPSL_postprint.pdf
Autor:
Wim Degruyter, Michele Prestifilippo, Stefano Corradini, Emilio Pecora, Massimo Musacchio, Malvina Silvestri, Simona Scollo, Costanza Bonadonna, Eduardo Rossi, Giuseppe Carparelli, Carmelo Cassisi, Emilio Biale, Luca Merucci, Raffaello Cioni
Publikováno v:
Remote Sensing, Vol. 11, No 2987 (2019) pp. 1-18
Remote Sensing
Remote Sensing; Volume 11; Issue 24; Pages: 2987
Remote Sensing
Remote Sensing; Volume 11; Issue 24; Pages: 2987
During explosive eruptions, emergency responders and government agencies need to make fast decisions that should be based on an accurate forecast of tephra dispersal and assessment of the expected impact. Here, we propose a new operational tephra fal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82712014a54c68ab1e31c88b495c2479
https://doi.org/10.3390/rs11242987
https://doi.org/10.3390/rs11242987