Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Malte Jochmann"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Permafrost is widespread in the High Arctic, including the Norwegian archipelago of Svalbard. The uppermost permafrost intervals have been well studied, but the processes at its base and the impacts of the underlying geology have been largely overloo
Externí odkaz:
https://doaj.org/article/71b11ef9c5264413b6221f790398aca5
Publikováno v:
Polar Research, Vol 32, Iss 0, Pp 1-19 (2013)
The study deals with environmental changes during the Paleocene–Eocene Thermal Maximum (PETM) and its background conditions in Spitsbergen through analysis of benthic foraminiferal assemblages (FA) in a section drilled in the Paleogene Central Basi
Externí odkaz:
https://doaj.org/article/4eabbfe2458f4940bdc96a0579194bfb
Autor:
Kim Senger, Matthijs Nuus, Niels Balling, Peter Betlem, Tom Birchall, Hanne H. Christiansen, Harald Elvebakk, Sven Fuchs, Malte Jochmann, Peter Klitzke, Kirsti Midttømme, Snorre Olaussen, Christophe Pascal, Nil Rodes, Aleksey Shestov, Aleksandra Smyrak-Sikora, Peter James Thomas
Publikováno v:
Senger, K, Nuus, M, Balling, N, Betlem, P, Birchall, T, Christiansen, H H, Elvebakk, H, Fuchs, S, Jochmann, M, Klitzke, P, Midttømme, K, Olaussen, S, Pascal, C, Rodes, N, Shestov, A, Smyrak-Sikora, A & Thomas, P J 2023, ' The subsurface thermal state of Svalbard and implications for geothermal potential ', Geothermics, vol. 111, 102702 . https://doi.org/10.1016/j.geothermics.2023.102702
Geothermics
Geothermics
Svalbard is a High Arctic Archipelago at 74–81°N and 15–35 °E under the sovereignty of Norway. All settlements in Svalbard, including the capital of Longyearbyen (population 2400), currently have isolated energy systems with coal or diesel as t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e65cf1eef4f056bc53b7aeeaaf1852a4
https://pure.au.dk/portal/da/publications/the-subsurface-thermal-state-of-svalbard-and-implications-for-geothermal-potential(4b83029e-8271-4064-a126-2f866ca58832).html
https://pure.au.dk/portal/da/publications/the-subsurface-thermal-state-of-svalbard-and-implications-for-geothermal-potential(4b83029e-8271-4064-a126-2f866ca58832).html
The polar regions are particularly sensitive to modern climate change. Despite the Arctic being home to isolated societies and vulnerable ecosystems, little is known about landscape and ecosystem response to climate change beyond short historical rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63afb6882ba2e0a495bb46ca3de82d05
https://doi.org/10.5194/egusphere-egu23-12414
https://doi.org/10.5194/egusphere-egu23-12414
Autor:
Snorre Olaussen, Sten-Andreas Grundvåg, Kim Senger, Ingrid Anell, Peter Betlem, Thomas Birchall, Alvar Braathen, Winfried Dallmann, Malte Jochmann, Erik P. Johannessen, Gareth Lord, Atle Mørk, Per T. Osmundsen, Aleksandra Smyrak-Sikora, Lars Stemmerik
Publikováno v:
Geological Society, London, Memoirs. 57
The Svalbard Composite Tectono-Sedimentary Element (SCTSE) is located on the northwestern corner of the Barents Shelf and comprises a Carboniferous–Pleistocene sedimentary succession. Due to Cenozoic uplift, the succession is subaerially exposed in
Autor:
Malte Jochmann, Rakul Maria Johannessen, Julian Janocha, Aleksandra Smyrak-Sikora, Simon J. Buckley, Isabelle Lecomte, Sten-Andreas Grundvåg, Lilith Kuckero, Rafael Kenji Horota, Thomas Birchall, Sarah M. Cohen, Kei Ogata, Peter Betlem, Kim Senger, Snorre Olaussen
Publikováno v:
Geoscience Communication
Senger, K, Betlem, P, Grundväg, S A, Horota, R K, Buckley, S J, Smyrak-Sikora, A, Jochmann, M M, Birchall, T, Janocha, J, Ogata, K, Kuckero, L, Johannessen, R M, Lecomte, I, Cohen, S M & Olaussen, S 2021, ' Teaching with digital geology in the high Arctic : Opportunities and challenges ', Geoscience Communication, vol. 4, no. 3, pp. 399-420 . https://doi.org/10.5194/gc-4-399-2021
Geoscience Communication, Vol 4, Pp 399-420 (2021)
Senger, K, Betlem, P, Grundväg, S A, Horota, R K, Buckley, S J, Smyrak-Sikora, A, Jochmann, M M, Birchall, T, Janocha, J, Ogata, K, Kuckero, L, Johannessen, R M, Lecomte, I, Cohen, S M & Olaussen, S 2021, ' Teaching with digital geology in the high Arctic : Opportunities and challenges ', Geoscience Communication, vol. 4, no. 3, pp. 399-420 . https://doi.org/10.5194/gc-4-399-2021
Geoscience Communication, Vol 4, Pp 399-420 (2021)
The Covid-19 pandemic occurred at a time of major revolution in the geosciences – the era of digital geology. Digital outcrop models (DOMs) acquired from consumer drones, processed using user-friendly photogrammetric software and shared with the wi
Autor:
Emily Koenders, Pim Kaskes, Niels de Winter, Malte Jochmann, Bas van de Schootbrugge, Martin Ziegler
Publikováno v:
Vrije Universiteit Brussel
Vrije Universiteit Amsterdam
Vrije Universiteit Amsterdam
Glendonites are calcite pseudomorphs, that form after the mineral ikaite. Their occurrence in sediments is typically seen as an indication of cold environmental conditions, even when found in predetermined greenhouse climates (Zhou et al., 2015). How
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::81fe481c0459077241179ce0cc42507d
https://doi.org/10.5194/egusphere-egu22-12047
https://doi.org/10.5194/egusphere-egu22-12047
Permafrost has become an increasingly important subject in the High Arctic archipelago of Svalbard. However, whilst the uppermost permafrost intervals have been well studied, the processes at its base and the impacts of the underlying geology have be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df2b8f49139a8b3335b69c9183b02158
https://doi.org/10.5194/tc-2021-226
https://doi.org/10.5194/tc-2021-226
A complex tectonic history and global climate change has influenced the land masses bordering the Arctic ocean. On land tectonic movement affects runoff patterns, local hydology such as increased precipitation and local surface elevation, which again
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f731898e9414ea0bbc93da846c869b55
https://doi.org/10.5194/egusphere-egu21-16340
https://doi.org/10.5194/egusphere-egu21-16340
Autor:
Cornelia Spiegel, Frank Lisker, Patrick Monien, Paul B. O'Sullivan, Katrin Meier, Karsten Piepjohn, Malte Jochmann
Prior to break up of Greenland and Svalbard, the Wandel sea basin with Carboniferous to Cenozoic deposits formed in eastern North Greenland. These deposits were affected by the last major period of Arctic tectonism, the Eocene Eurekan deformation. Vi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53c83760968443a81d85402e1c8692f9
https://doi.org/10.5194/egusphere-egu21-15213
https://doi.org/10.5194/egusphere-egu21-15213