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

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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Tollefsen, I. (1994). Dronning Maud Land (V. Sand, Ed.). Mortensen. https://doi.org/oai:nb.bibsys.no:999429985614702202 URN:NBN:no-nb_digibok_2009042804042

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Winther, J.-G. (1994). Spectral bi-directional reflectance of snow and glacier ice measured in Dronning Maud Land, Antarctica. Annals of Glaciology, 20, 1–5. https://doi.org/10.3189/1994AoG20-1-1-5

Visible and near-infrared spectral reflectances of snow and superimposed ice were measured in Dronning Maud Land, Antarctica, during the 1992-93 austral summer. Spectral-reflectance curves of both snow and superimposed ice remain high ( > 80%) in the visible region. A pronounced decrease in reflectance appears in the near-infrared, especially for superimposed ice. Superimposed ice with a 1 cm thick surface layer of ice-bound snow crystals had a considerably higher reflectance than superimposed ice containing only a few snow crystals. Furthermore, these data prove that snow and superimposed ice reflect solar radiation specularly and suggest that the anisotropy strengthens with increasing wavelengths. Integrated in-situ reflectances corresponding to Landsat TM bands 1-4 show that TM band 1 is least affected, whereas TM band 4 is most affected by anisotropy. Furthermore, the anisotropy increases with increasing off-nadir viewing angles up to an angle corresponding to 90°-θs (θs = solar elevation). For a 15° off-nadir sensor-observation angle, the average snow reflectance for TM bands 1--4 is about 10% higher than at nadir. Similarly, the apparent reflectance can be more than 50% higher than the nadir reflectance for larger observation angles. Consequently, if satellite-derived reflectances are going to be considered as absolute values, a topographic-correction model is needed to correct for the effects of anisotropy.

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Barr, S. (1993). Norwegian Antarctic whaling seen through the eye of the camera. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 177–189). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Barthelmess, K. (1993). A century of German interests in modern whaling, 1860s-1960s. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 121–138). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Basberg, B. L. (1993). Survival against all odds? Shore station whaling at South Georgia in the Pelagic. Era, 1925-1960. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 157–167). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Bucher-Nurminen, K., & Ohta, Y. (1993). Granulites and garnet–cordierite gneisses from Dronning Maud Land, Antarctica. Journal of Metamorphic Geology, 11(5), 691–703. https://doi.org/https://doi.org/10.1111/j.1525-1314.1993.tb00181.x

The central sector of Mühlig-Hofmannfjellet (3°E/71°S) in western Dronning Maud Land (East Antarctic shield) is dominated by large intrusive bodies of predominantly orthopyroxene-bearing quartz syenites (charnockites). Metasedimentary rocks are rare; however, two distinct areas with banded gneiss–marble–quartzite sequences of sedimentary origin were found during the Norwegian Antarctic Research Expedition NARE 1989/90. Cordierite-bearing metapelitic gneisses from two different localities contain the characteristic mineral assemblage: cordierite + garnet + biotite + K-feldspar + plagioclase + quartz ± sillimanite ± spinel. Thermobarometry indicates equilibration conditions of about 650°C and 4 kbar. Associated orthopyroxene–garnet granulites, on the other hand, revealed pressures of about 8 kbar and temperatures of 750°C. The earlier granulite facies metamorphism is not well preserved in the cordierite gneisses as a result of excess K-feldspar combined with interaction with an H2O-rich fluid phase, probably released by the cooling intrusives. These two features allowed the original high-grade K-feldspar + garnet assemblages to recrystallize as cordierite–biotite–sillimanite gneisses, completely re-equilibrating them. Phase relationships indicate that the younger metamorphic event occurred in the presence of a fluid phase that varied in composition between the lithologies.

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Ekra, S. I. S. (1993). Den farlige isen i Antarktis. Norges teknisk-naturvitenskapelige universitet SINTEF. https://gemini.no/2011/03/den-farlige-isen-i-antarktis/

All is i antarktiske havområder er flerårig under den antarktiske sommeren. Slik is er særlig sterk og hard og smelter ikke. I store bølger får de farlige stykkene stor fart. Treffer de en båt, skjer det med stor kraft.

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Headland, R. K. (1993). Geographical discoveries in Antarctica by the whaling industry. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 191–202). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Høgvard, K. (1993). Nature environment map: Gjelsvikfjella and Western Mühlig-Hofmannfjella, Dronning Maud Land, Antarctica (Y. Ohta, T. Engelskjøn, F. Mehlum, & L. Sømme, Eds.). Norsk Polarinstitutt. https://data.npolar.no/map/archive/ad4d2b9a-496e-579c-b7f1-35e407279399

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Husby, J., & Kolltveit, B. (1993). Hvalfangstlæge for 40 år siden. Norsk sjøfartsmuseum. Årsberetning, 1993, 65–108. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2019051381059_001 URN:NBN:no-nb_digitidsskrift_2019051381059_001

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Kristensen, M. (1993). Dager i Antarktis: om folk og forskning, og en ekspedisjon litt utenom det vanlige. Grøndahl Dreyer. https://urn.nb.no/URN:NBN:no-nb_digibok_2012032738071

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Magdahl, J. (1993). Kapittel 3 - Arbeidsløsheten. Kapittel 6 - Den lokale organisasjonen i 30-åra. In Framnæsarbeidernes historie (pp. 79–114, 147–165). Sandefjord jern og metallarbeiderforening. https://doi.org/oai:nb.bibsys.no:999327922434702202 URN:NBN:no-nb_digibok_2015062308200

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Sømme, L., Strømme, A., & Zachariassen, K. E. (1993). Notes on the ecology and physiology of the Antarctic oribatid mite Maudheimia wilsoni. Polar Research, 12(1), 21–25. https://doi.org/10.3402/polar.v12i1.6699

The oribatid mite Maudheimia wilsoni Dalenius was found to be numerous on the underside of stones at Jutulsessen (72-degrees-S, 3-degrees-E) in Dronning Maud Land, Antarctica. Daily temperature fluctuations of the microhabitat from as high as 19-degrees-C and to as low as -17-degrees-C were observed during the austral summer. Optimal activity of the mites occurred at 10-degrees-C. Even in January the mean supercooling point of adult mites was as low as - 30.8 +/- 4.7-degrees-C. Haemolymph osmolality ranged from 500 to 800 mOsmol and thermal hystersis freezing points from -4.7 to - 6.1-degrees-C. Adult mites had a mean water content of 43.6% and a water loss rate of 0.12 mug h-1 at 15-degrees-C and 10% relative humidity.

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Syvertsen, E. E., & Kristiansen, S. (1993). Ice algae during EPOS, leg 1: assemblages, biomass, origin and nutrients. Polar Biology, 13(1), 61–65. https://doi.org/10.1007/BF00236584

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Sæther, B.-E., Andersen, R., & Pedersen, H. C. (1993). Regulation of parental effort in a long-lived seabird an experimental manipulation of the cost of reproduction in the antarctic petrel, Thalassoica antarctica. Behavioral Ecology and Sociobiology, 33(3), 147–150. https://doi.org/10.1007/BF00216594

The fitness of a parent in an altricial bird species is likely to be a function of the proportion of resources allocated to offspring production in relation to the amount spent on its own survival. Here we report an experiment on the Antarctic petrel in which we manipulated the costs of rearing an offspring by placing small lead loads on the legs of one parent. The bird could then either decrease its own body reserves or reduce the food load to the chick. The manipulated birds decreased their food load and increased the feeding interval, compared with unmanipulated birds. Consequently, the rate of chick loss increased. No significant difference was found between the body weights of experimental and control birds during the experiment.

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Wexelsen, E. (1993). Vel blåst! : kommandør Chr. Christensens hvalfangstmuseum 75 år : 1917-1992 (Vol. 28). Kommandør Chr. Christensens hvalfangstmuseum. https://doi.org/oai:nb.bibsys.no:999304261504702202 URN:NBN:no-nb_digibok_2012080208202

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Wexelsen, E. (1993). Working Conditions and Work-related Injuries and Illnesses on board Norwegian Floating Factories after World War II. In B. L. Basberg, E. Wexelsen, & J. E. Ringstad (Eds.), Whaling and history : perspectives on the evolution of the industry (Vol. 29, pp. 139–156). Sandefjordmuseene. https://doi.org/oai:nb.bibsys.no:999328136904702202 URN:NBN:no-nb_digibok_2008010904042

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Jutulsessen: Fimbulheimen. (1992). Norsk Polarinstitutt. https://data.npolar.no/map/archive/772e18c0-9987-46bd-a598-9a72a9ef3136

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Bakka, D. (1992). Hvalfangsten : eventyret tar slutt. Krohn Johansen. https://doi.org/oai:nb.bibsys.no:999204380164702202 URN:NBN:no-nb_digibok_2007091704004

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