Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Rikke, Pedersen"'
Autor:
Michelle M. Parks, Freysteinn Sigmundsson, Vincent Drouin, Sigrún Hreinsdóttir, Andrew Hooper, Yilin Yang, Benedikt G. Ófeigsson, Erik Sturkell, Ásta R. Hjartardóttir, Ronni Grapenthin, Halldór Geirsson, Elisa Trasatti, Sara Barsotti, Rikke Pedersen, Páll Einarsson, Bergrún A. Óladóttir, Hildur M. Friðriksdóttir
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 4, Pp n/a-n/a (2024)
Abstract Unrest began in July 2021 at Askja volcano in the Northern Volcanic Zone (NVZ) of Iceland. Its most recent eruption, in 1961, was predominantly effusive and produced ∼0.1 km3 lava field. The last plinian eruption at Askja occurred in 1875.
Externí odkaz:
https://doaj.org/article/d85f8ea887504790a66318307fc7de2d
Autor:
Håvard Svanes Bertelsen, Rikke Pedersen, Olivier Galland, Karen Mair, Sigmundsson Freysteinn, Frank Guldstrand
Geodetic modelling has become an established procedure to interpret the dynamics of active volcanic plumbing systems. Most established geodetic models implemented for inverting geodetic data share similar physical assumptions: (1) the Earth's crust i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c625ff80eb0d4de4c38bcd27433d3d4
https://doi.org/10.5194/egusphere-egu21-13325
https://doi.org/10.5194/egusphere-egu21-13325
Publikováno v:
Lindquist, C, Nielsen, P N, Pedersen, R & N. Soltani, M 2018, Experimental Modelling of a Floating Offshore Wind Turbine . in Proceedings of the 23rd International Conference on Methods and Models in Automation and Robotics, MMAR ., 8485979, IEEE Press, pp. 327-332, 23rd International Conference on Methods & Models in Automation & Robotics, Miedzyzdroje, Poland, 27/08/2018 . https://doi.org/10.1109/MMAR.2018.8485979
MMAR
MMAR
Leading wind turbine manufacturers are increasingly looking at the possibilities of sending offshore wind turbines to deep seas. This can be done using a Floating Offshore Wind Turbine (FOWT). Therefore FOWT is an interesting and timely field of stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b185176d3560fd57bd7cd0a872fc4131
https://vbn.aau.dk/da/publications/f32a0461-1776-4109-a8e6-0c7158aa5fbc
https://vbn.aau.dk/da/publications/f32a0461-1776-4109-a8e6-0c7158aa5fbc
Autor:
Ásta Rut Hjartardóttir, Halldór Geirsson, Stéphanie Dumont, Þórdís Högnadóttir, Freysteinn Sigmundsson, Rikke Pedersen, Páll Einarsson, Matthew J. Roberts, Erik Sturkell, Magnús Tumi Guðmundsson, Vincent Drouin, Andrew Hooper, Elías Rafn Heimisson, Sigrún Hreinsdóttir, Kristín Vogfjörð, Talfan Barnie, Benedikt G. Ófeigsson, Ronni Grapenthin, Kristín Jónsdóttir, Michelle Parks
Improving our understanding of volcanic hazards requires better knowledge of the location, volume and properties of magma bodies in the roots of active volcanoes, as well as information on melt supply and magma transfer. This requires a good understa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ae27a04fdc867baed92cf3dd3a3025f
https://doi.org/10.1016/b978-0-12-809749-6.00011-x
https://doi.org/10.1016/b978-0-12-809749-6.00011-x
Autor:
Talfan Barnie, H.S. Bertelsen, Steffi Burchardt, Jim W. Cole, A.R. Cruden, Jonathan R.J. Davidson, Audray Delcamp, M. Detienne, Katherine J. Dobson, Vincent Drouin, Stéphanie Dumont, C.H. Eide, Páll Einarsson, O. Galland, Halldór Geirsson, Ronni Grapenthin, Darren M. Gravley, Magnús Guðmundsson, F. Guldstrand, Þórdís Högnadóttir, Ø.T. Haug, Elías Rafn Heimisson, Ásta Rut Hjartardóttir, Eoghan P. Holohan, Andy Hooper, Sigrún Hreinsdóttir, Kristín Jónsdóttir, Dougal A. Jerram, Janine L. Kavanagh, Ben M. Kennedy, Héctor A. Leanza, K. Mair, Dan J. Morgan, Sven Morgan, Benedikt G. Ófeigsson, E.M.R. Paguican, O. Palma, Matthew J. Pankhurst, Michelle Parks, Rikke Pedersen, S. Planke, S. Poppe, O. Rabbel, Matthew J. Roberts, B. Rogers, T. Schmiedel, Freysteinn Sigmundsson, A. Souche, J.B. Spacapan, John Stix, Erik Sturkell, Hugh Tuffen, Benjamin van Wyk de Vries, Maximillian van Wyk de Vries, Kristín Vogfjörð, Thomas R. Walter, R.F. Weinberg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::16deacdcf64c6e66845448fbe616dbde
https://doi.org/10.1016/b978-0-12-809749-6.00016-9
https://doi.org/10.1016/b978-0-12-809749-6.00016-9
Autor:
Rikke Pedersen, Erik Sturkell, Halldór Geirsson, Alan T. Linde, Freysteinn Sigmundsson, Selwyn Sacks, Halldór Ólafsson, Kristján Ágústsson, Páll Einarsson, Peter LaFemina
Publikováno v:
Journal of Volcanology and Geothermal Research. 256:78-86
Hekla is one of Iceland's most active volcanoes; its eruptions, characterized by surface fissuring and repeated lava flows during its post-glacial activity, have built up an 800 m high elongated mountain. Since 1970 it has erupted every ~ 10 years; t
Publikováno v:
The Leading Edge. 30:526-531
The 2010 eruption of Eyjafjallajökull has drawn increased attention to Iceland's Eastern Volcanic Zone (EVZ) due to the threat it poses to the heavily used air-traffic corridors of the northern Atlantic Ocean. Within the EVZ, Hekla is historically o
Publikováno v:
Earth and Planetary Science Letters. 281:14-26
article i nfo Extensional rifts are characterized by significant lateral variations in crustal rheology as lithospheric material cools and advects away from the rift axes. Nevertheless, most models used for modeling of crustal movements consist of ho
Autor:
Thóra Árnadóttir, Kurt L. Feigl, Freysteinn Sigmundsson, Carolina Pagli, Páll Einarsson, Rikke Pedersen
Publikováno v:
Earth and Planetary Science Letters. 259:24-33
Crustal deformation signals associated with the September 30–October 13, 1996 Gjalp subglacial eruption, Vatnajokull ice cap, Iceland, have been identified using interferometric analysis of Synthetic Aperture Radar images (InSAR) in areas outside t
Autor:
Rósa Ólafsdóttir, Ármann Höskuldsson, Karl Grönvold, Rikke Pedersen, Kristín Vogfjörð, Niels Oskarsson
Publikováno v:
Bulletin of Volcanology. 70:169-182
The 18th historic eruption of Hekla started on 26 February, 2000. It was a short-lived but intense event, emitting basaltic andesitic (55.5 wt% SiO2) pyroclastic fragments and lava. During the course of the eruption, monitoring was done by both instr