Antarktis-bibliografi er en database over den norske Antarktis-litteraturen.

Hensikten med bibliografien er å synliggjøre norsk antarktisforskning og annen virksomhet/historie i det ekstreme sør. Bibliografien er ikke komplett, spesielt ikke for nyere forskning, men den blir oppdatert.

Norsk er her definert som minst én norsk forfatter, publikasjonssted Norge eller publikasjon som har utspring i norsk forskningsprosjekt.

Antarktis er her definert som alt sør for 60 grader. I tillegg har vi tatt med Bouvetøya.

Det er ingen avgrensing på språk (men det meste av innholdet er på norsk eller engelsk). Eldre norske antarktispublikasjoner (den eldste er fra 1894) er dominert av kvalfangst og ekspedisjoner. I nyere tid er det den internasjonale polarforskninga som dominerer. Bibliografien er tverrfaglig; den dekker både naturvitenskapene, politikk, historie osv. Skjønnlitteratur er også inkludert, men ikke avisartikler eller upublisert materiale.

Til høyre finner du en «HELP-knapp» for informasjon om søkemulighetene i databasen. Mange referanser har lett synlige lenker til fulltekstversjon av det aktuelle dokumentet. For de fleste tidsskriftartiklene er det også lagt inn sammendrag.

Bibliografien er produsert ved Norsk Polarinstitutts bibliotek.

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isshelf

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Abstracts

Orheim, O., Østerhus, S., Melvold, K., Eiken, T., Thomsen, H. H., Winther, J.-G., & Bævre, H. (1997). Hot water drilling near Filchner station, Ronne ice shelf. In Report of the Norwegian Antarctic Research Expedition 1992/93 (Vol. 125, pp. 93–96). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173096

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Solås, M. K., & Eggenfellner, H. (1997). Changing mass balance of the Filchner ice shelf due to climate variations. In J.-G. (ed. ) Winther (Ed.), Report of the Norwegian Antarctic Research Expedition 1996/97 (Vol. 148, pp. 143–144). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173024

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Erlingsson, B., Gjessing, Y., Hamran, S. E., & Holmlund, P. (1994). Detailed studies of bottom freezing under an iceshelf and mapping of accumulation by use of multi-frequency pulse-aperture radar. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 43–46). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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Nøst, O. A., & Foldvik, A. (1994). A model of ice shelf-ocean interaction with application to the Filchner-Ronne and Ross Ice Shelves. Journal of Geophysical Research: Oceans, 99(C7), 14243–14254. https://doi.org/https://doi.org/10.1029/94JC00769

A simple analytical model has been developed to study the formation of Ice Shelf Water (ISW). ISW is assumed to flow as a buoyancy-driven layer underneath the ice shelf. A relation between potential temperature and salinity in the ISW layer is calculated from the mass and energy balance. This temperature-salinity relation is shown to depend only on the temperature and the salinity of the source water mass and to be practically independent of entrainment and melt rates. The model results are obtained without making any assumptions about entrainment and melt rates. The model is in good agreement with observations under the Ronne Ice Shelf, and it indicates that ISW in the Filchner Depression is formed from Western Shelf Water (WSW) with salinity higher than 34.75 practical salinity units. Such high-salinity water is only observed in the Ronne Depression in the western part of the continental shelf. This implies a circulation of WSW, under the Filchner-Ronne Ice Shelf, from the Ronne Depression into the Filchner Depression. Similarly, the model shows that the ISW observed under J9 at the Ross Ice Shelf has been formed from Low Salinity Shelf Water (LSSW) from the eastern parts of the Ross Sea continental shelf. LSSW must therefore circulate under the eastern parts of the Ross Ice Shelf.

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Solheim, A. (1994). Proximal sub ice-shelf sedimentation Jutulgryta, East Antarctica. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 29–33). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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Kuvaas, B., & Kristoffersen, Y. (1991). The Crary Fan: A trough-mouth fan on the Weddell Sea continental margin, Antarctica. Marine Geology, 97(3), 345–362. https://doi.org/https://doi.org/10.1016/0025-3227(91)90125-N

Multichannel seismic investigations show the presence of a large trough-mouth fan deposit on the continental margin in the southern Weddell Sea. A characteristic feature of the fan is relatively few, but large canyons and/or channels which appear to have been stable for long periods. Levees associated with the channels may reach thicknesses of more than 1 km. Drilling during ODP Leg 113 recorded the presence of glaciers in East Antarctica since early Oligocene time, and the seismic stratigraphic evidence suggests that the submarine fan is largely composed of glacigenic sediments. The channel-levee systems and complexes indicate several growth phases, apparently controlled by glacial/interglacial climate fluctuations, with maximum fan growth during glacial periods. The present interglacial period is characterized by strong and erosive flow of Ice Shelf Water running down the western slope of the fan and carrying only minor amounts of suspended matter. The fan is essentially sediment starved during interglacial periods. The dimensions of the channel-levee complexes and the persistent loci of sediment supply suggest that turbidite sedimentation resulted from melting of wet-based glaciers at or near the shelf edge, which has consequently prograded 70-80 km seaward.

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Solheim, A., Forsberg, C., & Pittenger, A. (1991). Stepwise Consolidation of Glacigenic Sediments Related to the Glacial History of Prydz Bay, East Antarctica. In J. Barron & B. Larsen (Eds.), Proceedings of the Ocean Drilling Program (Vol. 119, pp. 169–182). College station. https://doi.org/10.2973/odp.proc.sr.119.187.1991
Foldvik, A., Gammelsrød, T., Nordlund, N., & Nytun, K. (1990). Observations of ice shelf water at the southern Weddel sea shelf break. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 125–130). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Foldvik, A., Middleton, J. H., & Foster, T. D. (1990). The tides of the southern Weddell Sea. Deep Sea Research Part A. Oceanographic Research Papers, 37(8), 1345–1362. https://doi.org/https://doi.org/10.1016/0198-0149(90)90047-Y

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Kennett, M. (1990). Radio-echo investigations in Dronning Maud Land. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 75–79). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Orheim, O., Hagen, J. O., Østerhus, S., & Sætrang, A. (1990). Studies on, and underneath, the Ice Shelf Fimbulisen. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 59–73). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Schlosser, P., Bayer, R., Foldvik, A., Gammelsrød, T., Rohardt, G., & Münnich, K. O. (1990). Oxygen 18 and helium as tracers of ice shelf water and water/ice interaction in the Weddell Sea. Journal of Geophysical Research: Oceans, 95(C3), 3253–3263. https://doi.org/https://doi.org/10.1029/JC095iC03p03253

Oxygen 18 and helium isotope data from stations located in the Filchner Depression, on the continental slope of the southern Weddell Sea, and in the central Weddell Sea are presented and discussed. The 18O and 4He signals imprinted on the water circulating under the Filchner/Ronne Ice Shelf (Ice Shelf Water, or ISW) due to melting of glacial ice at the base of the ice shelf are traced across the sill separating the Filchner Depression from the Weddell Sea. Low δ18O values are correlated with high 4He concentrations in the ISW found in the Filchner Depression (minimum δ18O values: −0.8‰; maximum 4He concentrations: about 4.7×10−8 cm3 STP g−1). The fraction of glacial meltwater contained in the ISW found in the Filchner Depression is estimated to about 6 to 7‰. The 18O and helium isotope data from the overflowing shelf water component observed on the continental slope confirm the hypothesis that ISW contributes significantly to the Weddell Sea Bottom Water (WSBW). On the basis of a inultiparameter water mass analysis it is discussed which fraction of the WSBW originates from ISW and which other shelf waters potentially could contribute to WSBW.

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Lien, R., Solheim, A., Elverhøi, A., & Rokoengen, K. (1989). Iceberg scouring and sea bed morphology on the eastern Weddell Sea shelf, Antarctica. Polar Research, 7(1), 43–57. https://doi.org/10.3402/polar.v7i1.6829

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Foldvik, A., & Gammelsrød, T. (1988). Notes on Southern Ocean hydrography, sea-ice and bottom water formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 67(1), 3–17. https://doi.org/https://doi.org/10.1016/0031-0182(88)90119-8

The Southern Ocean circulation and sea-ice distribution is briefly described. The formation of extremely cold bottom water in the Weddell Sea and its relation to the floating Ronne-Filchner Ice Shelves is discussed. It is shown that a concentrated swift eroding bottom current with anomalous low ratio transports the cold and dense ice Shelf Water from the shelf towards large depths. Comments are made on possible implications of this process for the large-scale deep-water circulation and for the interpretation of sediment cores.

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Gjessing, Y., & Wold, B. (1986). Absolute movements, mass balance and snow temperatures of the Riiser-Larsenisen Ice Shelf, Antarctica. In Glaciological research on Riiser-Larsenisen and nearby ice-shelves in Antarctica (Vol. 187, pp. 23–31). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173516

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Orheim, O., & Drewry, D. (1986). Flow and thickness of Riiser-Larsenisen, Antarctica. In Glaciological research on Riiser-Larsenisen and nearby ice-shelves in Antarctica (Vol. 187, pp. 5–22). Norsk Polarinstitutt. http://hdl.handle.net/11250/173516

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Orheim, O., Gjessing, Y., Lunde, T., Repp, K., Wold, B., Clausen, H. B., & Liestøl, O. (1986). Oxygen isotopes and accumulation rates at Riiser-Larsenisen, Antarctica. In Glaciological research on Riiser-Larsenisen and nearby ice-shelves in Antarctica (Vol. 187, pp. 32–47). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173516

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Foldvik, A., Gammelsrød, T., Slotsvik, N., & Tørresen, T. (1985). Oceanographic conditions on the Weddell Sea Shelf during the German Antarctic Expedition 1979/80. Polar Research, 3(2), 209–226. https://doi.org/10.3402/polar.v3i2.6953

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Foldvik, A., Gammelsrød, T., & Tørresen, T. (1985). Physical oceanography studies in the Weddell Sea during the Norwegian Antarctic Research Expedition 1978/79. Polar Research, 3(2), 195–207. https://doi.org/10.3402/polar.v3i2.6952

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Nøst, O. A., & Østerhus, S. (1985). Impact of Grounded Icebergs on the Hydrographic Conditions Near the Filchner Ice Shelf. In Ocean, Ice, and Atmosphere: Interactions at the Antarctic Continental Margin (Vol. 75, pp. 267–284). American Geophysical Union. https://doi.org/https://doi.org/10.1029/AR075p0267

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Last update from database: 3/1/25, 3:17 AM (UTC)