Academic literature on the topic 'Isfjorden'

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Journal articles on the topic "Isfjorden"

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Bloshkina, E. V., and K. V. Filchuk. "The present water masses conditions of West Spitsbergen fjords." Arctic and Antarctic Research 64, no. 2 (2018): 125–40. http://dx.doi.org/10.30758/0555-2648-2018-64-2-125-140.

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The study is based on CTD measurements collected during Arctic cruises in Isfjorden including Billefjorden and Gronfjorden in summer between 2011 and 2017. The purpose of this paper is to describe the present state of fjords water masses. In the first part of the paper distributions of water masses in Isfjorden and Billefjorden in summer 2014–2017 and in Grönfjorden in summer 2011– 2017 are analyzed. In paper was shown that for Isfjorden and Grönfjorden there were 4 types of masses: surface water, intermediate water, transformed Atlantic water, and Atlantic water. In June 2014, was recorded the situation when Atlantic waters occupied the entire water area of Isfjord and Grönfjord. In summer in Billefjorden were identified 4 types of masses: surface water, intermediate water, local water, and winter water. In Isfjorden, new maximum temperature of Atlantic water was observed (6.85 °С) in summer 2016. It is greater on almost 0.5 °С than previous warmest peak in 2006. The maximum average values of water temperature, heat content in the upper 40 m layer were recorded in 2016. The summer 2016 was the warmest in Isfjorden, Billefjorden and Grönfjorden during the survey period.
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Muckenhuber, S., F. Nilsen, A. Korosov, and S. Sandven. "Sea ice cover in Isfjorden and Hornsund 2000–2014 by using remote sensing." Cryosphere Discussions 9, no. 4 (2015): 4043–66. http://dx.doi.org/10.5194/tcd-9-4043-2015.

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Abstract. A satellite database including 16 555 satellite images and ice charts displaying the area of Isfjorden, Hornsund and the Svalbard region has been established with focus on the time period 2000–2014. 3319 manual interpretations of sea ice conditions have been conducted, resulting in two time series dividing the area of Isfjorden and Hornsund into "Fast ice", "Drift ice" and open "Water". The maximum fast ice coverage of Isfjorden is > 40 % in the periods 2000–2005 and 2009–2011 and stays < 30 % in 2006–2008 and 2012–2014. Fast ice cover in Hornsund reaches > 40 % in all considered years, except for 2012 and 2014, where the maximum stays < 20 %. The mean seasonal cycles of fast ice in Isfjorden and Hornsund show monthly averaged values of less than 1 % between July and November and maxima in March (Isfjorden, 35.7 %) and April (Hornsund, 42.1 %) respectively. A significant reduction of the monthly averaged fast ice coverage is found when comparing the time periods 2000–2005 and 2006–2014. The seasonal maximum decreases from 57.5 to 23.2 % in Isfjorden and from 52.6 to 35.2 % in Hornsund. A new concept, called "days of fast ice coverage" (DFI), is introduced for quantification of the interannual variation of fast ice cover, allowing for comparison between different fjords and winter seasons. Considering the time period from 1 March until end of sea ice season, the mean DFI values for 2000–2014 are 33.1 ± 18.2 DFI (Isfjorden) and 42.9 ± 18.2 DFI (Hornsund). A distinct shift to lower DFI values is observed in 2006. Calculating a mean before and after 2006 yields a decrease from 50 to 22 DFI for Isfjorden and from 56 to 34 DFI for Hornsund.
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Muckenhuber, S., F. Nilsen, A. Korosov, and S. Sandven. "Sea ice cover in Isfjorden and Hornsund, Svalbard (2000–2014) from remote sensing data." Cryosphere 10, no. 1 (2016): 149–58. http://dx.doi.org/10.5194/tc-10-149-2016.

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Abstract. A satellite database including 16 555 satellite images and ice charts displaying the area of Isfjorden, Hornsund, and the Svalbard region has been established with focus on the time period 2000–2014. 3319 manual interpretations of sea ice conditions have been conducted, resulting in two time series dividing the area of Isfjorden and Hornsund into "fast ice" (sea ice attached to the coastline), "drift ice", and "open water". The maximum fast ice coverage of Isfjorden is > 40 % in the periods 2000–2005 and 2009–2011 and stays < 30 % in 2006–2008 and 2012–2014. Fast ice cover in Hornsund reaches > 40 % in all considered years, except for 2012 and 2014, where the maximum stays < 20 %. The mean seasonal cycles of fast ice in Isfjorden and Hornsund show monthly averaged values of less than 1 % between July and November and maxima in March (Isfjorden, 35.7 %) and April (Hornsund, 42.1 %), respectively. A significant reduction of the monthly averaged fast ice coverage is found when comparing the time periods 2000–2005 and 2006–2014. The seasonal maximum decreases from 57.5 to 23.2 % in Isfjorden and from 52.6 to 35.2 % in Hornsund. A new index, called "days of fast ice" (DFI), is introduced for quantification of the interannual variation of fast ice cover, allowing for comparison between different fjords and winter seasons. Considering the time period from 1 March until end of the sea ice season, the mean DFI values for 2000–2014 are 33.1 ± 18.2 DFI (Isfjorden) and 42.9 ± 18.2 DFI (Hornsund). A distinct shift to lower DFI values is observed in 2006. Calculating a mean before and after 2006 yields a decrease from 50 to 22 DFI for Isfjorden and from 56 to 34 DFI for Hornsund. Fast ice coverage generally correlates well with remote-sensing sea surface temperature and in situ air temperature. An increase of autumn ocean heat content is observed during the last few years when the DFI values decrease. The presented sea ice time series can be utilized for various climate effect studies linked to, e.g. glacier dynamics, ocean chemistry, and marine biology.
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Frank, Lukas, Marius Opsanger Jonassen, Teresa Remes, Florina Roana Schalamon, and Agnes Stenlund. "IWIN: the Isfjorden Weather Information Network." Earth System Science Data 15, no. 9 (2023): 4219–34. http://dx.doi.org/10.5194/essd-15-4219-2023.

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Abstract. In an effort led by the University Centre in Svalbard (UNIS), with support from the Norwegian Meteorological Institute (MET Norway), the Isfjorden Weather Information Network (IWIN) is under development in the Isfjorden region in central Svalbard. The network substantially expands upon the relatively sparse existing operational network of weather stations and consists of compact and cost-efficient all-in-one weather stations permanently installed at lighthouses around Isfjorden and on board small tourist cruise ships trafficking the fjord from spring to autumn. All data from the network until June 2023, as presented in this paper, can be found at https://doi.org/10.5281/zenodo.8137588 (Frank et al., 2023b). New data become freely available in near-real time via MET Norway's data portals (https://doi.org/10.21343/ebrw-w846, Frank et al., 2023a). The IWIN data are highly valuable for scientific purposes such as atmospheric boundary layer research, the validation and development of numerical weather prediction models, and assimilation in these, as well as the planning and safe conduction of outdoor activities in the region.
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Fredriksen, Stein, Tove M. Gabrielsen, Maia R. Kile, and Knut Sivertsen. "Benthic algal vegetation in Isfjorden, Svalbard." Polar Research 34, no. 1 (2015): 25994. http://dx.doi.org/10.3402/polar.v34.25994.

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Nilsen, Frank, Ragnheid Skogseth, Juni Vaardal-Lunde, and Mark Inall. "A Simple Shelf Circulation Model: Intrusion of Atlantic Water on the West Spitsbergen Shelf." Journal of Physical Oceanography 46, no. 4 (2016): 1209–30. http://dx.doi.org/10.1175/jpo-d-15-0058.1.

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AbstractBarotropic flow along depth contours is found in accordance with standard geostrophic theory. A numerical model is developed that studies the deviation from such a flow. The model gives a good approximation of the dynamical processes on the West Spitsbergen Shelf (WSS) and shows that the West Spitsbergen Current (WSC), the main gateway of Atlantic water (AW) toward the Arctic, connects more easily to the Isfjorden Trough than anywhere else along the shelf. The circulation of AW in the troughs along the WSS is here named the Spitsbergen Trough Current (STC). From hydrographical and ocean current observations it is evident that the STC is primarily barotropic and driven by the sea surface height. A connection between the along-coast wind stress and the STC is established, and it is demonstrated how the increased occurrence of winter cyclones in Fram Strait during January–February accelerates and widens the WSC. Ultimately, this results in a strengthened STC and dominance of AW on the WSS. The STC represents a slower route of AW toward the Arctic Ocean and a large heat transport toward the West Spitsbergen fjords during winter (0.2–0.4 TW toward Isfjorden). Heat flux estimates show that half of the AW heat loss in the Isfjorden Trough is due to heat loss to the surrounding water masses, while the rest is lost to the atmosphere. Sea ice production along West Spitsbergen has been reduced, or even nonexistent, in some fjords since 2006. Here, the authors argue that this is a consequence of the strong southerly wind periods along the WSS during winter.
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Vihma, Timo, Tiina Kilpeläinen, Miina Manninen, et al. "Characteristics of Temperature and Humidity Inversions and Low-Level Jets over Svalbard Fjords in Spring." Advances in Meteorology 2011 (2011): 1–14. http://dx.doi.org/10.1155/2011/486807.

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Air temperature and specific humidity inversions and low-level jets were studied over two Svalbard fjords, Isfjorden and Kongsfjorden, applying three tethersonde systems. Tethersonde operation practices notably affected observations on inversion and jet properties. The inversion strength and depth were strongly affected by weather conditions at the 850 hPa level. Strong inversions were deep with a highly elevated base, and the strongest ones occurred in warm air mass. Unexpectedly, downward longwave radiation measured at the sounding site did not correlate with the inversion properties. Temperature inversions had lower base and top heights than humidity inversions, the former due to surface cooling and the latter due to adiabatic cooling with height. Most low-level jets were related to katabatic winds. Over the ice-covered Kongsfjorden, jets were lifted above a cold-air pool on the fjord; the jet core was located highest when the snow surface was coldest. At the ice-free Isfjorden, jets were located lower.
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Losi, Niccolò, Piotr Markuszewski, Martin Rigler, et al. "Anthropic Settlements’ Impact on the Light-Absorbing Aerosol Concentrations and Heating Rate in the Arctic." Atmosphere 14, no. 12 (2023): 1768. http://dx.doi.org/10.3390/atmos14121768.

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Light-absorbing aerosols (LAA) impact the atmosphere by heating it. Their effect in the Arctic was investigated during two summer Arctic oceanographic campaigns (2018 and 2019) around the Svalbard Archipelago in order to unravel the differences between the Arctic background and the local anthropic settlements. Therefore, the LAA heating rate (HR) was experimentally determined. Both the chemical composition and high-resolution measurements highlighted substantial differences between the Arctic Ocean background (average eBC concentration of 11.7 ± 0.1 ng/m3) and the human settlements, among which the most impacting appeared to be Tromsø and Isfjorden (mean eBC of 99.4 ± 3.1 ng/m3). Consequently, the HR in Isfjorden (8.2 × 10−3 ± 0.3 × 10−3 K/day) was one order of magnitude higher than in the pristine background conditions (0.8 × 10−3 ± 0.9 × 10−5 K/day). Therefore, we conclude that the direct climate impact of local LAA sources on the Arctic atmosphere is not negligible and may rise in the future due to ice retreat and enhanced marine traffic.
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9

Roy, Srikumar, Martin Hovland, Riko Noormets, and Snorre Olaussen. "Seepage in Isfjorden and its tributary fjords, West Spitsbergen." Marine Geology 363 (May 2015): 146–59. http://dx.doi.org/10.1016/j.margeo.2015.02.003.

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Bour, Aurélien. "La récolte de plantes vivantes in situ et la mise en culture en jardin botanique en pratique, l'exemple de la flore vasculaire du Spitzberg." Bulletin de la Société d'Histoire Naturelle et d'Ethnologie de Colmar 75 (June 7, 2018): 27–34. https://doi.org/10.5281/zenodo.14802182.

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RÉSUMÉLa flore du Svalbard est riche de 184 espèces vasculaires. Cette flore est considérée commeexceptionnellement riche eu égard à l’emplacement de l’archipel. À l’occasion de l’expéditionau Spitzberg menée, en juillet 2018, conjointement par l’association Sibbaldia et la Sociétéd’Histoire naturelle et d’Ethnographie de Colmar, un programme de culture et de conservationex situ de plantes vasculaires a été mis en place en collaboration avec le jardin d’altitudedu Chitelet dans le massif vosgien. Les explorations botanistes ont été menées sur les zonesles plus accessibles de la rive sud de l’Isfjorden. Au total, ce travail a permis de récolteret de mettre en culture 134 échantillons correspondant à 91 espèces, soit environ 300 potsen culture. À partir d’une mise en culture le 23 juillet, au jardin d’altitude du Chitelet, la quasitotalitédes végétaux ont présenté une croissance au mois de septembre. À ce jour, seulementquatre espèces n’ont présenté aucun signe de reprise et ont péri.MOTS-CLÉS : Spitzberg, Isfjorden, botanique, récolte, plantes vivantes, jardin botanique,éducation, conservation, recherche.ABSTRACTThe flora of Svalbard accounts 184 vascular species. This flora is considered as exceptionallyrich despite to the northern location of the archipelago. During the expeditionto Spitzberg - conducted in July 2018 jointly by the Sibbaldia association andthe Society of Natural History and Ethnography of Colmar - a program of conservationand ex situ culture of vascular plants has was set up in collaboration with the altitudebotanical garden of Chitelet in the Vosges mountains. Fieldworks were carried outon the most accessible areas of the South bank of the Isfjorden. In total, this workallowed to collect and put in culture 134 samples corresponding to 91 species,about 300 pots in culture. Since July 23, almost all vascular plants showed growthin September. To date, only four species have shown no signs of recovery and haveperished.KEYWORDS
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Book chapters on the topic "Isfjorden"

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Forwick, Matthias, and Tore O. Vorren. "Submarine Mass Wasting in Isfjorden, Spitsbergen." In Submarine Mass Movements and Their Consequences. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-2162-3_63.

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Rudenko, Olga. "Upper Holocene Stratigraphy and Pollen Case Study of Isfjorden, West Spitsbergen (Svalbard, Norway)." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_250.

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Conference papers on the topic "Isfjorden"

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Kruss, Aleksandra, Jozef Wiktor, Jozef Wiktor, and Agnieszka Tatarek. "Acoustic detection of macroalgae in a dynamic Arctic environment (Isfjorden, West Spitsbergen) using multibeam echosounder." In 2019 IEEE Underwater Technology (UT). IEEE, 2019. http://dx.doi.org/10.1109/ut.2019.8734323.

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Reports on the topic "Isfjorden"

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Kruss, A., J. Wiktor, A. Tatarek, and J. Wiktor. Mapping macroalgae beds and environmental factors for understanding the impact of climate change in the Arctic - a case study from Isfjorden (West Spitsbergen). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/305877.

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