Gotowe bibliografie tematyczne / Iceland Sea

Spis treści

  1. Artykuły w czasopismach
  2. Rozprawy doktorskie
  3. Książki
  4. Części książek
  5. Streszczenia konferencji
  6. Raporty organizacyjne

Gotowa bibliografia na temat „Iceland Sea”

Autor: Grafiati
Data publikacji: 2 czerwca 2025
Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Iceland Sea"

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Arnalds, O., H. Olafsson, and P. Dagsson-Waldhauserova. "Quantification of iron-rich volcanogenic dust emissions and deposition over the ocean from Icelandic dust sources." Biogeosciences 11, no. 23 (2014): 6623–32. http://dx.doi.org/10.5194/bg-11-6623-2014.

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Abstract. Iceland has extremely active dust sources that result in large-scale emissions and deposition on land and at sea. The dust has a volcanogenic origin of basaltic composition with about 10% Fe content. We used two independent methods to quantify dust emission from Iceland and dust deposition at sea. Firstly, the aerial extent (map) of deposition on land was extended to ocean areas around Iceland. Secondly, surveys of the number of dust events over the past decades and calculations of emissions and sea deposition for the dust storms were made. The results show that total emissions range
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Arnalds, O., H. Olafsson, and P. Dagsson-Waldhauserova. "Quantification of iron-rich volcanogenic dust emissions and deposition over ocean from Icelandic dust sources." Biogeosciences Discussions 11, no. 4 (2014): 5941–67. http://dx.doi.org/10.5194/bgd-11-5941-2014.

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Abstract. Iceland has extremely active dust sources that result in large scale emissions and deposition on land and sea. The dust has volcanogenic origin of basaltic composition with about 10 % Fe content. We used two independent methods to quantify dust emission from Iceland and dust deposition on sea. Firstly, aerial extent (map) of deposition on land was extended to ocean areas around Iceland. Secondly, survey of number of dust events over the past decades and calculations of emissions and sea deposition for the dust storms were made. The results show total emissions range from 30.5 (dust e
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Magnússon, Bjarni Már, and Snjólaug Árnadóttir. "Iceland’s Territorial Sea Baselines, Volcanic Eruptions and Sea Level Rise." Yearbook of Polar Law Online 15, no. 1 (2024): 3–19. https://doi.org/10.1163/22116427_015010002.

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Abstract Volcanic eruptions can have various consequences, including in the field of the international law of the sea. This article addresses the impact that two volcanic eruptions had on the baselines for measuring the breadth of Iceland’s territorial sea. First, the impact of the eruption in 1918 in Katla was addressed by the Supreme Court of Iceland in 1922 which confirmed a district court decision stating that the territorial sea line was not a fixed or determined line on the sea but changed with avulsions and accretions. Second, the sudden appearance of the volcanic island Surtsey in 1963
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Hanna, Edward, Trausti Jónsson, Jon Ólafsson, and Hedinn Valdimarsson. "Icelandic Coastal Sea Surface Temperature Records Constructed: Putting the Pulse on Air–Sea–Climate Interactions in the Northern North Atlantic. Part I: Comparison with HadISST1 Open-Ocean Surface Temperatures and Preliminary Analysis of Long-Term Patterns and Anomalies of SSTs around Iceland." Journal of Climate 19, no. 21 (2006): 5652–66. http://dx.doi.org/10.1175/jcli3933.1.

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Abstract A new comprehensive record of long-term Icelandic sea surface temperature measurements, which have been updated and filled in with reference to air temperature records, is presented. The new SST series reveal important features of the variability of climate in Iceland and the northern North Atlantic. This study documents site histories and possible resulting inconsistencies and biases, for example, changes in observing sites and instruments. A new 119-yr continuous time series for north Iceland SST is presented, which should prove particularly useful for investigating air–sea ice inte
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Kjetil, Våge, Moore G.W.K., Jónsson Steingrímur, and Valdimarsson Héðinn. "Water mass transformation in the Iceland Sea." Deep Sea Research Part 1: Oceanographic Research Papers Volume 101,, July 2015, (2015): 98–109. https://doi.org/10.1016/j.dsr.2015.04.001.

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The water mass transformation that takes place in the Iceland Sea during winter is investigated using historical hydrographic data and atmospheric reanalysis fields. Surface densities exceeding σθ=27.8kg/m3, and hence of sufficient density to contribute to the lower limb of the Atlantic Meridional Overturning Circulation via the overflows across the Greenland-Scotland Ridge, exist throughout the interior Iceland Sea east of the Kolbeinsey Ridge at the end of winter. The deepest and densest mixed layers are found in the northwest Iceland Sea on the outskirts of the basin׳s cyclonic
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Olafsson, Kristinn, Sigurdur M. Einarsson, John Gilbey, et al. "Origin of Atlantic salmon (Salmo salar) at sea in Icelandic waters." ICES Journal of Marine Science 73, no. 6 (2015): 1525–32. http://dx.doi.org/10.1093/icesjms/fsv176.

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Abstract The origin and life history of 186 Atlantic salmon caught at sea within Icelandic waters were investigated using microsatellites to assess the origin and scales and otoliths to assess freshwater and sea age. A total of 184 samples were aged using scales or otolithes or both. Most of the samples were from individuals in their first year at sea (72.8%). The freshwater age varied from 1 to 5 years with an average of 2.6 years. The most common freshwater age was 2 years (42%), with a further substantial proportion of 3-year-old fish (28%). Genetic assignment of individual fish to their mo
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Blechschmidt, A. M., J. E. Kristjánsson, H. Ólafsson, J. F. Burkhart, and Ø. Hodnebrog. "Aircraft-based observations and high-resolution simulations of an Icelandic dust storm." Atmospheric Chemistry and Physics Discussions 12, no. 3 (2012): 7949–84. http://dx.doi.org/10.5194/acpd-12-7949-2012.

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Abstract. The first aircraft-based observations of an Icelandic dust storm are presented. The measurements were carried out over the ocean near Iceland's south coast in February 2007. This dust event occurred in conjunction with an easterly barrier jet of more than 30 m s−1. The aircraft measurements show high particle mass mixing ratios in an area of low wind speeds in the wake of Iceland near the coast, decreasing abruptly towards the jet. Simulations from the Weather Research and Forecasting Model coupled with Chemistry (WRF/Chem) indicate that the measured high mass mixing ratios and obser
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Blechschmidt, A. M., J. E. Kristjánsson, H. Ólafsson, J. F. Burkhart, Ø. Hodnebrog, and P. D. Rosenberg. "Aircraft-based observations and high-resolution simulations of an Icelandic dust storm." Atmospheric Chemistry and Physics 12, no. 22 (2012): 10649–66. http://dx.doi.org/10.5194/acp-12-10649-2012.

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Abstract. The first aircraft-based observations of an Icelandic dust storm are presented. The measurements were carried out over the ocean near Iceland's south coast in February 2007. This dust event occurred in conjunction with an easterly barrier jet of more than 30 m s−1. The aircraft measurements show high particle mass mixing ratios in an area of low wind speeds in the wake of Iceland near the coast, decreasing abruptly towards the jet. Simulations from the Weather Research and Forecasting Model coupled with Chemistry (WRF/Chem) indicate that the measured high mass mixing ratios and obser
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Risebrobakken, Bjørg, Mari F. Jensen, Helene R. Langehaug, et al. "Buoyancy forcing: a key driver of northern North Atlantic sea surface temperature variability across multiple timescales." Climate of the Past 19, no. 5 (2023): 1101–23. http://dx.doi.org/10.5194/cp-19-1101-2023.

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Abstract. Analyses of observational data (from year 1870 AD) show that sea surface temperature (SST) anomalies along the pathway of Atlantic Water transport in the North Atlantic, the Norwegian Sea and the Iceland Sea are spatially coherent at multidecadal timescales. Spatially coherent SST anomalies are also observed over hundreds of thousands of years during parts of the Pliocene (5.23–5.03, 4.63–4.43, and 4.33–4.03 Ma). However, when investigating CMIP6 (Coupled Model Intercomparison Project 6) SSP126 (Shared Socioeconomic Pathway) future scenario runs (next century) and other Pliocene time
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Guðmundsdóttir, Esther Ruth, Jón Eiríksson, and Guðrún Larsen. "Holocene marine tephrochronology on the Icelandic shelf: An overview." Jökull 62, no. 1 (2012): 53–72. http://dx.doi.org/10.33799/jokull2012.62.053.

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Currently the Late-glacial and Holocene marine tephrochronology on the shelf around Iceland comprises 130 tephra layers from 30 sediment cores ranging in age from 15,000 years cal. BP to AD 1947. A vast majority of the cores and tephra layers are from the North Iceland shelf. Much fewer tephra layers have been found on the South and West Iceland shelf. The early Holocene Saksunarvatn ash and Vedde Ash are the only tephra layers identified on all investigated shelf areas. For the last 15,000 years correlated tephra layers from the shelf sediments around Iceland to their terrestrial counterparts
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Rozprawy doktorskie na temat "Iceland Sea"

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Brader, Martin David. "Postglacial relative sea-level changes and the deglaciation of northwest Iceland." Thesis, Durham University, 2015. http://etheses.dur.ac.uk/11317/.

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Iceland provides an important opportunity to investigate relative sea-level (RSL) changes and Last Glacial Maximum (LGM) glaciation in a sensitive area of the North Atlantic. This project employs new and existing RSL data, coupled with glacio-isostatic adjustment (GIA) modelling, to resolve the current debates surrounding the extent of the LGM Icelandic ice sheet (IIS). Robust understanding of the LGM IIS is important, because there are two markedly different maximum and minimum ice loading scenarios, with very different implications for global thermohaline circulation. Previous studies of gla
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Jóhannsdóttir, Guðrún Elín. "Methods for Coastal Flooding Risk Assessments : An Application in Iceland." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-396970.

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Flood risk increases with rising sea levels and coastal settlements need to adapt to this increasing risk. For that, hazard and risk assessments are an important step. Coastal floods have caused problems in Iceland in the past and are thought to do so in the future as well. Therefore, a coastal flooding risk as- sessment needs to be made for Iceland. A risk assessment is currently in the early steps of preparation and a fitting method needs to be developed. To facilitate the process, an overview of the methods used in neighbouring countries is provided here and the suitability of the methods f
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Bjarnadóttír, Hólmfríður. "SEA in the Context of Land-Use Planning : The application of the EU directive 2001/42/EC to Sweden, Iceland and England." Licentiate thesis, Karlskrona : Blekinge Institute of Technology, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:bth-00417.

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The thesis addresses the introduction of a supra-national instrument; a European directive on Strategic Environmental Assessment (SEA) into national contexts of land-use planning in three countries; Sweden, Iceland and England. The directive ”On the assessment of the effects of certain plans and programmes on the environment” was agreed upon by the European Commission on the 21st of June 2001 and was to be transposed to national legislation by 21st of June 2004. The introduction of these requirements meant that the countries needed to make legal adjustments and implement it at the different le
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Bjarnadóttir, Hólmfríður. "SEA in the context of land-use planning : the application of the EU directive 2001/42/EC to Sweden, Iceland and England /." Karlskrona : Department of Spatial Planning, School of Technoculture, Humanities and Planning, Blekinge Institute of Technology, 2008. http://www.bth.se/fou/Forskinfo.nsf/allfirst2/432b3042e2fe636ac12574c6004e1c40?OpenDocument.

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Preston, John Ian. "Geomorphology of Viking and medieval harbours in the North Atlantic." Thesis, University of Edinburgh, 2018. http://hdl.handle.net/1842/31430.

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The aim of this thesis is to understand the role of geomorphological change in the abandonment of Norse harbours in the North Atlantic. Nodes of maritime activities that were established by Norse settlers during the Scandinavian Viking Age often developed into important towns and cities. Some of these, however, disappeared for unknown reasons. Norse harbours in the North Atlantic varied in scale. They ranged from small landing beaches used by small boats for local use through to much larger anchorages handling considerable trade and being important nodes on the transatlantic trading network. C
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Fish, Stephanie. "Icelandic Glacial Ice Volume Changes and its Contribution to Sea Level Rise since the Little Ice Age Maximum." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-296216.

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Satellite imagery and volume-area scaling are used to asses the glacier area and ice volume of Iceland from the Little Ice Age maximum to present day, obtaining a final result in sea level rise between 1890 - 2015. The Little Ice Age was a time of regional cooling, with glaciers reaching their maximum extent (~1890 for Iceland) with warming and glacier retreat after this period ended. Ice volume estimates are important to know due to their relevance in potential sea level rise calculations. Understanding both of these estimations for Iceland connects the impact a changing climate has on region
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Schreck, Michael [Verfasser], Ruediger [Akademischer Betreuer] Stein, and Karin [Akademischer Betreuer] Zonneveld. "Biostratigraphy and Paleoenvironment in the Neogene of the High Northern Latitudes - Insights from the palynomorph record of ODP Hole 907A in the Iceland Sea / Michael Schreck. Gutachter: Ruediger Stein ; Karin Zonneveld. Betreuer: Ruediger Stein." Bremen : Staats- und Universitätsbibliothek Bremen, 2012. http://d-nb.info/1071993860/34.

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Walker, Angela Jane. "Rhyolite volcanism at Öræfajökull volcano, S.E. Iceland : a window on Quaternary climate change." Thesis, University of Manchester, 2012. https://www.research.manchester.ac.uk/portal/en/theses/rhyolite-volcanism-at-oraefajokull-volcano-se-iceland--a-window-on-quaternary-climate-change(c00888e4-53a6-4fd0-ad54-110be2a42952).html.

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Öræfajökull is an ice-capped stratovolcano situated in the south east of Iceland which has developed throughout the mid to late Quaternary. It has erupted basaltic and rhyolitic lavas during interglacial and glacial periods, many of which display strong physical evidence of volcano-ice interaction. This makes Öræfajökull an ideal location to reconstruct terrestrial palaeo-environments. The area of Goðafjall and Hrútsfjall is one of a small number of rhyolitic depositional centres situated on the south west flanks of the volcano and is the first rhyolitic area of Öræfajökull to be mapped in det
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Edblom, Lena. "Långhus i Gene : teori och praktik i rekonstruktion." Doctoral thesis, Umeå University, Archaeology and Sami Studies, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-248.

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<p>Under åren 1977–89 bedrev arkeologiska institutionen vid Umeå universitet en forskningsundersökning av en boplats från äldre järnålder på Genesmon i Själevad socken, norra Ångermanland. Under åren 1991–99 rekonstruerades delar av gården i Gene fornby, ett hundratal meter därifrån. Denna avhandling behandlar uppbyggnad och inredning av ett av gårdens långhus, hus II, samt den treskeppiga byggnadstypens konstruktion och funktion i en större kontext. Syftet med avhandlingen är att beskriva växelverkan mellan teori och praktik i rekonstruktion, att beskriva rekonstruktionsarbete som en föränder
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Nováková, Barbora. "Tulení kůže: interpretace islandské pohádky a jejich motivů ve vztahu k staroseverskému symbolickému rámci." Master's thesis, 2020. http://www.nusl.cz/ntk/nusl-436615.

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This work presents an interpretation of icelandic narrative about the Seal Skin with regard to the Old Norse symbolic frame, so the possible paralel motifs and motivic "cores" could arise, even in spite of the temporal period between the origin of our primary text and the origin of Old Norse myths and sagas. The approach of this work is based in structural theories and tools used by Claude Lévi-Strauss, where these tools help us identify the basic narrative units called mythemes: primarily they include characters, objects and settings. The basic principle of founding these mythemes in differen
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Książki na temat "Iceland Sea"

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Páll, Stefánsson, ed. Visions of Iceland: Scenes and surprises from land and sea. Iceland Review, 1999.

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Group, Boston Foreign Affairs, and Icelandic Association for Western Co-operation., eds. Iceland, Nato, and security in the Norwegian Sea: A report from a conference in Reykjavík, Iceland, 12th-13th March, 1987. Icelandic Association for Western Co-Operation, 1987.

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Sigurðardóttir, Yrsa. The silence of the sea. Thorpe, 2015.

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Canada. Dept. of Fisheries and Oceans. Scotia-Fundy Region. Biological Sciences Branch. Atlas of the biology and distribution of the Sea scallop Placopecten magellanicus and Iceland scallop Chlamys islandica in the Northwest Atlantic. Dept. of Fisheries and Oceans, Biological Sciences Branch, 1993.

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Moss, Stephen R. Tick-borne viruses in icelandic seabird colonies. Icelandic Museum of Natural History, 1986.

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Office, Great Britain Hydrographic. Arctic pilot: Iceland, Jan Mayen, Bjørnøja, Svalbard, and the east coast of Greenland together with the adjacent seas. 8th ed. Hydrographer of the Navy, 1996.

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Jóhannesson, Guðni Th. Troubled waters: Cod War, fishing disputes, and Britain's fight for the freedom of the high seas, 1948-1964. North Atlantic Fisheries History Association, 2007.

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Spencer, Scott. Willing. Ecco, 2008.

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Spencer, Scott. Willing. Ecco, 2008.

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Rune, Skjoldal Hein, World Ocean Circulation Experiment, and Joint Global Ocean Flux Study., eds. MARE COGNITUM: Science plan for research on marine ecology of the Nordic Seas (Greenland, Norwegian, Iceland Seas) 1993-2000 : a regional GLOBEC program with contributions also to WOCE and JGOFS. [s.n., 1993.

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Części książek na temat "Iceland Sea"

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Magnússon, Bjarni Már. "Iceland and seabed mining." In Routledge Handbook of Seabed Mining and the Law of the Sea. Routledge, 2023. http://dx.doi.org/10.4324/9780429426162-36.

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Hansom, James D., and David J. Briggs. "Sea-Level Change in Vestfirđir, North West Iceland." In Glaciology and Quaternary Geology. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3150-6_6.

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Ingólfsson, Agnar. "Colonization of floating seaweed by pelagic and subtidal benthic animals in southwestern Iceland." In Island, Ocean and Deep-Sea Biology. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-1982-7_17.

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Larrington, Carolyne. "“Þá fær Þorbirni svá mjǫk at hann grætr”: Emotionality in the Sagas of East Iceland." In Emotional Alterity in the Medieval North Sea World. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-33965-3_3.

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Thors, Kjartan, and Guðrún Helgadóttir. "Evidence from South West Iceland of Low Sea Level in Early Flandrian Times." In Glaciology and Quaternary Geology. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3150-6_7.

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Wastl, Maria, Johann Stötter, and Chris J. Caseldine. "Sea Ice-Climate-Glacier Relationships in Northern Iceland since the Nineteenth Century: Possible Analogues for the Holocene." In History and Climate. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4757-3365-5_9.

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McCarthy, Conor. "Icelandic Literature." In Love, Sex & Marriage in the Middle Ages, 2nd ed. Routledge, 2022. http://dx.doi.org/10.4324/9781003147404-27.

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Wyatt, Ian. "Narrative Function of Landscape in the Old Icelandic Family Sagas." In Land, Sea and Home. Routledge, 2024. http://dx.doi.org/10.4324/9781003580249-19.

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Jóhannesson, Gunnar Thór. "Sailing the Seas of Tourism: Past, Present and Future Mobilities on the Margins." In Arctic Encounters. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-41344-5_5.

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AbstractThe objective of the chapter is to trace how places are created through mobilities and tourism performances. The discussion is based on relational ontology, framing tourism as an ordering that enacts realities rather than a neatly defined industry or a sector. Hence, instead of thinking about tourism as a practice that happens within a pre-defined space it is illustrated how tourism encounters produce space. The chapter sets out from two encounters between tourists and a ship grounded at the shoreline at the shoreline of Skápadalur in Patreksfjörður, in the southern part of the Westfjo
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Fohrmann, Hermann, Jan O. Backhaus, Frank Blaume, et al. "Modern Ocean Current-Controlled Sediment Transport in the Greenland-Iceland-Norwegian (GIN) Seas." In The Northern North Atlantic. Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/978-3-642-56876-3_9.

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Streszczenia konferencji na temat "Iceland Sea"

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Karlsdottir, Sigrun N., Ingolfur O. Thorbjornsson, Kolbrun R. Ragnarsdottir, and Asbjorn Einarsson. "Corrosion Testing of Heat Exchanger Tubes in Steam from the IDDP-1 Exploratory Geothermal Well in Krafla, Iceland." In CORROSION 2014. NACE International, 2014. https://doi.org/10.5006/c2014-4152.

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Abstract The IDDP-1 well in the Krafla geothermal field in Iceland is the first well in the Icelandic deep drilling project. The superheated steam from the well is extremely hot (450°C) with a 120 bar pressure at the wellhead. The IDDP-1 steam contains acid gas and is highly corrosive when it condenses. A test unit with eight different material types of heat exchanger tubes was set up in order to investigate the possibility of using the IDDP-1 steam directly for heat exchangers without prior removal of silica, sulfur and acid gases. The tube materials were three types of stainless steel, two t
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Csáki, Ioana, Radu Stefanoiu, Sigrun Nanna Karlsdottir, et al. "Mechanically Alloyed CoCrFeNiMo High Entropy Alloy Behavior in Geothermal Steam." In CORROSION 2019. NACE International, 2019. https://doi.org/10.5006/c2019-13239.

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Abstract A multicomponent High Entropy Alloy (HEA) CoCrFeNiMo processed in solid state, by mechanical alloying, was tested for corrosion in geothermal environment in the Reykjanes Geothermal Power Plant in Iceland. An electron scanning microscope (SEM) and X-ray Energy Dispersive Spectroscopy (EDS) were used to investigate the samples before and after corrosion test. A weight loss method was also used to measure the corrosion rate of the CoCrFeNiMo high entropy alloy. And inspection of the specimen after the exposure in the geothermal environment revealed sulfur and oxygen corrosion products.
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Csaki, Ioana, Sigrun Nanna Karlsdottir, Ciprian Alexandru Manea, Radu Stefanoiu, Roxana Trusca, and Victor Geanta. "Microstructural Study of the Corrosion Effect on AlCrFeNiMn Multicomponent Alloy Tested in Geothermal Environment." In CORROSION 2017. NACE International, 2017. https://doi.org/10.5006/c2017-08916.

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Abstract A multicomponent High Entropy Alloy (HEA) AlCrFeNiMn processed with vacuum arc remelting procedure was tested for corrosion in geothermal environment in the Reykjanes Geothermal Power Plant in Iceland. Microstructural and chemical composition analysis of the material was performed before and after testing in the geothermal steam with an electron scanning microscope (SEM) and X-ray Energy Dispersive Spectroscopy (X-EDS). A weight loss method was also used to measure the corrosion rate of the AlCrFeNiMn high entropy alloy. The results showed that the uniform corrosion rate was quite hig
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Csáki, Ioana, Radu Stefanoiu, Sigrun Nanna Karlsdottir, and Laura Elena Geambazu. "Corrosion Behavior in Geothermal Steam of CoCrFeNiMo High Entropy Alloy." In CORROSION 2018. NACE International, 2018. https://doi.org/10.5006/c2018-11139.

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Abstract A multicomponent High Entropy Alloy (HEA) CoCrFeNiMo processed with vacuum arc remelting procedure was tested for corrosion in geothermal environment in the Reykjanes Geothermal Power Plant in Iceland. Microstructural and chemical composition analysis of the material was performed before and after testing in the geothermal steam with an electron scanning microscope (SEM) and X-ray Energy Dispersive Spectroscopy (X-EDS). A weight loss method was also used to measure the corrosion rate of the CoCrFeNiMo high entropy alloy. The results showed that the uniform corrosion rate low, on avera
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Ragnarsdottir, Kolbrun R., Aðalsteinn Arnbjornsson, Sigrun N. Karlsdottir, and Helen O. Haraldsdottir. "Preliminary Corrosion Testing of Explosive Clad Materials in Geothermal Environment." In CORROSION 2018. NACE International, 2018. https://doi.org/10.5006/c2018-11154.

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Abstract Geothermal steam commonly contains CO2 and H2S dissolved gases which are corrosive substances. An explosive welding technique was used for preparing samples of clad carbon steel material with different corrosion resistant alloys (CRAs) for testing in geothermal environment. A test unit was connected to a high temperature geothermal well, KJ-34, at the Krafla geothermal system in Iceland for in-situ corrosion testing. The steam was around 190°C with 14 bar pressure, pH value 8.57 and contained dissolved gases, including H2S and CO2. For this preliminary experiment austenitic stainless
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Ragnarsdottir, Kolbrun R., Sigrun N. Karlsdottir, Kristjan Leosson, et al. "Corrosion Testing of Coating Materials for Geothermal Turbine Application." In CORROSION 2017. NACE International, 2017. https://doi.org/10.5006/c2017-09185.

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Abstract Development is needed for new materials and technology to extend the life and reliability of material surfaces used in geothermal steam turbines. A test unit was designed so that steam flows directly from the wellhead into the test unit through a nozzle where the steam is flashed at high velocity on the target area. This setup simulates the effect of erosion and erosion-corrosion in geothermal steam turbines in Iceland. Well HE-29 at Hellisheiði geothermal power plant was selected for testing. The steam from the wellhead had temperatures around 210°C at 18 bar pressure and it containe
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Thorhallsson, Andri Isak, Sigrun Nanna Karlsdottir, and Andri Stefansson. "Corrosion Testing of UNS S31603 in Simulated HT Geothermal Environment at Boiling, Superheated and Condensation Conditions." In CORROSION 2019. NACE International, 2019. https://doi.org/10.5006/c2019-13195.

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Abstract Corrosion testing of austenitic stainless steel, UNS S31603 (AISI 316L), was conducted in flow-through reactors during early stages of lab setup development with the aim to obtain a superheated steam environment with H2S/CO2/HCl at 350°C and 10 bars. The test fluid; aqueous solution with the corrosive species was preheated, boiled and superheated in preheater before entering the reactors. But due to regular high-volume injection periods of the aqueous solution into the preheater and insufficient thermal insulation surrounding the test unit, a liquid droplet transportation into the rea
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Iqbal, Muhammad Amjad, Andrei Anghel, and Mihai Datcu. "Ice Cover Delineation Over Devon Iceland Using Sentinel Polarimetric SAR and Optical Data." In 2023 IEEE International Workshop on Metrology for the Sea; Learning to Measure Sea Health Parameters (MetroSea). IEEE, 2023. http://dx.doi.org/10.1109/metrosea58055.2023.10317415.

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Atlason, Reynir Smari, and Runar Unnthorsson. "Operation and Maintenance in Icelandic Geothermal Power Plants: Structure and Hierarchy." In ASME 2013 Power Conference. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/power2013-98207.

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The Icelandic geothermal industry can be traced back to 1908 and has developed an extensive knowledge from that time. Currently, seven geothermal power plants are operating on the island. The plants are operated and maintained efficiently by relatively few engineers. The power plants generally prefer marine engineers who have worked as chief engineers on fishing vessels. Marine engineers are preferred in the Icelandic geothermal sector because of their education and mentality learned while working on the sea. Teamwork, resourcefulness, proactive thinking and the will to assist with jobs beyond
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Sund, Sveinung M., Thomas Berg Iversen, Magnus S. Hansen, et al. "Simulation of Oil Production from Homogenous North Sea Reservoirs with Inflow Control using OLGA/Rocx." In The 58th Conference on Simulation and Modelling (SIMS 58) Reykjavik, Iceland, September 25th – 27th, 2017. Linköping University Electronic Press, 2017. http://dx.doi.org/10.3384/ecp17138188.

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Raporty organizacyjne na temat "Iceland Sea"

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Ramsey, Andree L., Heather H. Furey, and Amy S. Bower. Overturning of the Subpolar North Atlantic Program (OSNAP): RAFOS Float Data Report June 2014 - January 2019. Woods Hole Oceanographic Institution, 2022. http://dx.doi.org/10.1575/1912/29540.

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The Overturning in the Subpolar North Atlantic Program (OSNAP) is an international effort started in 2014 dedicated to achieving a better understanding of the link between dense-water formation and the meridional overturning circulation in the high-latitude North Atlantic. Moorings, gliders, and subsurface acoustically-tracked RAFOS floats have been used to collect temperature, salinity, and current data across the Labrador Sea, Irminger Sea, Reykjanes Ridge, Iceland Basin, Rockall-Hatton Plateau, and Rockall Trough. The specific objective of the OSNAP float program is to gather information on
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Kopf, Achim, and Sina Löschke. New findings on sub-seabed storage of carbon dioxide: The six most important outcomes of AIMS³ research. CDRmare, 2025. https://doi.org/10.3289/cdrmare.44.

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In the CDRmare research consortium AIMS³, experts have spent the past three years investigating under which conditions carbon dioxide (CO2) dissolved in seawater could be stored in the young basalt crust south of Iceland. In addition, they have developed new, deep-sea-capable sensors and monitoring systems for measuring the mineralisation of the stored CO2 and assessing the environmental soundness of such a potential deep-sea storage project.
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Petersen, Guðrún. Alviðruhamrar – Meteorological conditions. Icelandic Meteorological Office, 2025. https://doi.org/10.33112/damc5680.

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This report is written for EP Power Minerals ehf. that is planning activities in in SoutheastIceland. Themeteorological conditions inMýrdalssandur and Alviðruhamrar in SoutheastIceland are analysed using observations from two automatic long-term weather stations and reanalysis data from the CARRA reanalysis project. The emphasis is on the wind conditions. The climate of the region is mild and wet. There are three main wind directions, northerly, easterly and southwesterly. Winds from the north are in general dry and winds form the east wet. However, depending on the general weather conditions
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A deep-sea experiment on carbon dioxide storage in oceanic crust. CDRmare, 2022. http://dx.doi.org/10.3289/cdrmare.21.

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On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers currently investigate the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in the seawate
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Knowledge summary, A deep-sea experiment on carbon dioxide storage in oceanic crust. CDRmare, 2022. http://dx.doi.org/10.3289/cdrmare.20.

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On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers are currently investigating the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in the s
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A deep-sea experiment on carbon dioxide storage in oceanic crust - Version 2. CDRMare, 2023. http://dx.doi.org/10.3289/cdrmare.21_v2.

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Factsheet: On Iceland, water enriched with carbon dioxide has been injected into the upper ocean crust since 2014 – and successfully. The carbon dioxide mineralises within a short time and is firmly bound for millions of years. However, since ocean crust only rises above sea level in a few places on Earth, researchers currently investigate the option of injecting carbon dioxide into ocean regions where huge areas of suitable basalt crust lie at medium to great water depths. One possible advantage: In the deep sea subsurface, the carbon dioxide would either be stable as a liquid or dissolve in
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