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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Abstracts

Jaworowski, Z., Segalstad, T. V., & Hisdal, V. (1992). Atmospheric CO₂ and global warming: a critical review (Vol. 119). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999210527154702202 URN:NBN:no-nb_digibok_2007112100107

View on urn.nb.no
Jaworowski, Z., Segalstad, T. V., & Ono, N. (1992). Do glaciers tell a true atmospheric CO2 story? Science of The Total Environment, 114, 227–284. https://doi.org/10.1016/0048-9697(92)90428-U

Until 1985 most studies of CO2 in gas inclusions in pre-industrial ice indicated that CO2 concentrations (up to 2450 ppm) were higher than the current atmospheric level. After 1985, lower pre-industrial CO2 values were reported, and used as evidence for a recent man-made CO2 increase. The errors in these revised values, however, are of a similar magnitude to the apparent increase in atmospheric CO2 level. The assumptions used in estimating lower CO2 values in past atmospheres have been: no liquid phase in polar ice; younger age of air than of ice due to free gas exchange between deep firn and the atmosphere; and no change in composition of air inclusions. These assumptions are shown to be invalid. Liquid saline water exists in ice at low temperatures, even below −70°C; airtight ice layers are ubiquitous in Antarctic firn; and more than 20 physico-chemical processes operating in situ and in ice cores contribute to the alteration of the chemical composition of air inclusions. The permeable ice sheet with its capillary liquid network acts as a sieve which redistributes elements, isotopes, and micro-particles. Thirty-six to 100% of air recovered from old ice is contaminated by recent atmospheric air during field and laboratory operations. The value of ∼290 ppm, widely accepted from glacier studies for the pre-industrial atmospheric CO2 level, apparently results from: invalid assumptions; processes in ice sheets; artifacts in ice cores; and arbitrary rejection of high readings. To date, glaciological studies are not able to provide a reliable reconstruction of either the CO2 level in pre-industrial and ancient atmospheres or paleoclimates. Instead these studies have led to a widely accepted false dogma of man-made climatic warming. This dogma may have enormous negative impact on our common future.

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Kverndal, A.-I., Elvebakk, A., Jaworowski, Z., & Hansson, R. (1990). Virkninger av klimaendringer i polarområdene : bidrag til den interdepartementale klimautredningen (Vol. 62). Norsk Polarinstitutt. http://hdl.handle.net/11250/173224

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Kristoffersen, Y., & Aalerud, J. (1988). Aeromagnetic reconnaissance over the Riiser-Larsen Ice Shelf, east Antarctica. Polar Research, 6(1), 123–128. https://doi.org/10.3402/polar.v6i1.6852

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Orheim, O. (1985). Iceberg discharge and the mass balance of Antarctica. National Academy 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.

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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

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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. (1981). The glaciers of Bouvetøya. In Bouvetøya, South Atlantic Ocean : results from the Norwegian Antarctic Research Expeditions 1976/77 and 1978/79 (Vol. 175, pp. 79–84). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Foldvik, A., Gammelsrød, T., & Gjessing, Y. (1980). Measurements of oscillations and flexure of icebergs. Annals of Glaciology, 1, 29–30. https://doi.org/10.3189/S0260305500016918
Foldvik, A., Gammelsrød, T., & Gjessing, Y. (1980). Measurements of the radiation temperature of Antarctic icebergs and the surrounding surface water. Annals of Glaciology, 1, 19–22. https://doi.org/10.3189/S026030550001689X
Orheim, O. (1978). Glaciological studies by Landsat imaginery of perimeter of Dronning Maud Land, Antarctica. In Results from Norwegian Antarctic Research 1974-1977 (Vol. 169, pp. 69–80, ill. fig.). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173650

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Orheim, O. (1978). Hvorfor er de Antarktiske isfjell så store? Naturen, 102(6), 277–280.
Orheim, O. (1977). Global glacier mass balance variations during the past 300 years (M. J. Dunbar, Ed.). Arctic Institute of North America.
Gjessing, Y. (1972). Mass transport of Jutulstraumen ice stream in Dronning Maud Land. In Norsk Polarinstitutt. Årbok 1970 (pp. 227–232). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172754

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Orheim, O. (1972). A 200-Year Record of Glacier Mass Balance at Deception Island, Southwest Atlantic Ocean, and Its Bearing on Models of Global Climatic Change (Vol. 42). The Ohio State University. https://kb.osu.edu/handle/1811/51272

View on kb.osu.edu
Lunde, T. (1965). On the firn temperatures and glacier flow in Dronning Maud Land. In Norsk Polarinstitutt. Årbok 1963 (pp. 7–24). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172799

View on brage.npolar.no

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