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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Topic

glasiologi

Results 336 resources

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Abstracts

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. (1986). Glaciological research on the Norwegian Antarctic Research Expedition (NARE) 1984/85. Filchner-Ronne Ice Shelf Programme. Report, 3, 64–67.
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

View on hdl.handle.net
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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Gjessing, Y. (1985). Meteorological and glaciological studies in Dronning Maud Land. In Report of the Norwegian Antarctic research expedition (NARE) 1984/85 (Vol. 22, pp. 63–66). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173240

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Jonsson, S. (1985). Geomorphological and glaciological observations in Vestfjella, Dronning Maud Land. In Report of the Norwegian Antarctic research expedition (NARE) 1984/85 (Vol. 22, pp. 83–88). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173240

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Kristensen, M., & Orheim, O. (1985). Iceberg research and other glaciological studies from K/V “Andenes.” In Report of the Norwegian Antarctic research expedition (NARE) 1984/85 (Vol. 22, pp. 127–138). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173240

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Moberg, J. (1985). På ekspedisjon til Sørpolen. Norsk barneblad, 98(3), 50–52. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2015071581236_001

View on urn.nb.no
Orheim, O. (1985). Iceberg discharge and the mass balance of Antarctica. National Academy Press.
Orheim, O. (1985). Isfjell og isbreer i Antarktis. Det norske videnskaps-akademi. Årbok, 1985(1985), 101–103.
Elverhøi, A., & Maisey, G. (1983). Glacial erosion and morphology of the eastern and southeastern Weddell Sea shelf (R. L. Oliver, P. R. James, & J. B. Jago, Eds.). Cambridge University Press.
Kristensen, M. (1983). Iceberg calving and deterioration in Antarctica. Progress in Physical Geography: Earth and Environment, 7(3), 313–328. https://doi.org/10.1177/030913338300700301

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Kristensen, M., & Squire, V. A. (1983). Automatic collection of tilt and strain data from tabular icebergs. Annals of Glaciology, 4, 147–151. https://doi.org/10.3189/S0260305500005383
Kristensen, M., & Squire, V. A. (1983). Modelling of antarctic tabular icebergs in ocean waves. Annals of Glaciology, 4, 152–157. https://doi.org/10.3189/S0260305500005395

The prediction of the motions of a tabular iceberg in a seaway is a problem which cannot be solved with a simple approach. The main difficulty lies in the size and mass of the iceberg, which produce frequency-dependent hydrodynamical effects as it moves in the water. Specifically, any solution must take into account both the added inertia and the generation of surface waves caused by the motions of the berg. Early attempts at modelling, which did not include these terms, could not accurately predict the complicated response behaviour seen in field data. In this paper we discuss some modifications to a two-dimensional simulation of floating bodies in waves, which must be applied when the motions and the hydro-dynamical pressures beneath tabular icebergs are required.
Wadhams, P., Kristensen, M., & Orheim, O. (1983). The response of Antarctic icebergs to ocean waves. Journal of Geophysical Research: Oceans, 88(C10), 6053–6065. https://doi.org/10.1029/JC088iC10p06053

The heave, tilt, and strain responses of three Antarctic tabular icebergs to ocean waves were measured during a 1980–1981 cruise of HMS Endurance to the South Atlantic. The three icebergs, located near the South Sandwich and South Orkney islands, were instrumented with accelerometers, tiltmeters, and wire strainmeters, while a Waverider buoy was used to record the ocean wave field. The thickness of the icebergs was surveyed by a helicopter-borne radio echo sounder. The heave response occurred mainly at the swell period but with outbreaks of bobbing which lasted for a few cycles at a resonant period (about 40 s), which agreed well with the predictions of a numerical finite element model. The roll response occurred mainly at a long resonant period (40–50 s), which again agreed well with the model, but there was also a significant response at ocean wave periods (5–20 s), which exceeded predictions. The strain response had a component at very long periods, which is unexplained by theory, while the surface strain at ocean wave periods agreed with the simple analytical model of Goodman et al. (1980). Using this model it is possible to predict a wave height and period that will cause breakup of the icebergs, and we conclude that swell-induced breakup is likely to occur during major storms in the open southern ocean.

View on agupubs.onlinelibrary.wiley.com
Kristensen, M., Squire, V. A., & Moore, S. C. (1982). Tabular icebergs in ocean waves. Nature, 297(5868), 669–671. https://doi.org/10.1038/297669a0

View on doi.org
Orheim, O. (1982). Radio echo-sounding of Riiser-Larsenisen (abstract only). Annals of Glaciology, 3, 355. https://doi.org/10.3189/S0260305500003347
Orheim, O., & Govorukha, L. S. (1982). Present-day glaciation in the South Shetland Islands. Annals of Glaciology, 3, 233–238. https://doi.org/10.3189/S0260305500002834
Orheim, O., & Govorukha, L. S. (1982). Present-day glaciation in the South Shetland Islands. Annals of Glaciology, 3, 233–238. https://doi.org/10.3189/S0260305500002834

This paper presents mass-balance results from Deception Island for 1968–69 to 1973–74, from King George Island for the balance years 1969–70 and 1970–71, and from Livingston Island from 1971–72 to 1973–74. The accumulation areas of all localities are in the soaked fades, with a firn/ice transition at King George Island at 12 to 20 m depth. Of the glaciers studied, only “Gl” on Deception Island terminates wholly on land and has a relatively large ablation area. The mass-balance curves are similar for King George Island and Livingston Island, with equilibrium lines at around 150 m elevation. “Gl“ on Deception Island has more negative summer balances, and the equilibrium line ranged from 275 to 370 m during the six balance years. Here, there were no years of positive net mass balance, and large negative net values during the 1970–71 to 1972–73 balance years. This resulted from a lowered albedo caused by ash from the August 1970 eruption. Ash layers from the Deception Island eruptions are also observed on Livingston Island and King George Island, where they form stratigraphic markers in the accumulation areas of the glaciers. Annual balance variations from 1957–58 to 1970–71, based on stratigraphic studies at Deception Island and King George Island, show good correlations, indicating that the variations reflect changes in regional climate.
Orheim, O., Wadhams, P., & Kristensen, M. (1982). Iceberg response to sea state (abstract only). Annals of Glaciology, 3, 357. https://doi.org/10.3189/S0260305500003360

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