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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Full bibliography 2,884 resources

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Abstracts

Barr, S. (1994). Norske offentlige samlinger med kulturhistorisk polarmateriale (Vol. 134). Norsk polarinstitutt. https://doi.org/oai:nb.bibsys.no:999509121234702202 URN:NBN:no-nb_digibok_2008012400002

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Baughman, T. H. (1994). Before the heroes came : Antarctica in the 1890s. University of Nebraska Press.
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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Fothergill, A. (1994). Antarktis: verdens siste villmark. Cappelen. https://urn.nb.no/URN:NBN:no-nb_digibok_2009042300018

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Gammelsrød, T. (1994). Water mass distribution and tides along the Filchner-Ronne ice shelf: preleminary [sic] results from the Norwegian Antarctic Expedition 1992/93. Filchner-Ronne Ice Shelf Programme. Report, 7, 42–46.
Gammelsrød, T., Foldvik, A., Nøst, O. A., Foldvik, Ø., Anderson, L. G., Fogelqvist, E., Olsson, K. A., Tanhua, T., Jones, E. P., & Østerhus, S. (1994). Distribution of Water Masses on the Continental Shelf in the Southern Weddell Sea. In The Polar Oceans and Their Role in Shaping the Global Environment (Vol. 85, pp. 159–176). https://doi.org/10.1029/GM085p0159

Water properties on the continental shelf in the southern Weddell Sea observed during NARP 92/93 are presented. The station distribution includes a section close to the floating ice shelf from the Filchner Depression to the Antarctic Peninsula. Temperature, salinity, oxygen, silicate, CFC-ll and CFC-12 distributions are shown. Melting under the ice shelves, circulation systems, residence times, sediment/water interactions and bottom water formation are discussed. Ice Shelf Water (ISW), which is formed by cooling and melting below the floating ice shelf, seems to be about 10 years older than its parent water mass, which indicates the residence time below the ice shelf. The average melting rate below the Filchner Ronne ice shelf, based on the volume flux of ISW in the Filchner Depression is estimated to be 0.1 m/year. Compared with earlier observations considerable changes were found in the water characteristics and distribution: The temperature of the Weddell Deep Water has increased 0.7°C since 1977. Western Shelf Water, usually dominating the bottom layers in the Filchner Depression and on the Berkner Shelf, was found only in the Ronne Depression.
Gjessing, Y., & Erlingsson, B. (1994). Chemical fractionation of sea salt in snow. In Report of the Norwegian Antarctic Research Expedition 1991/92 (Vol. 124, pp. 35–41). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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Hasle, G. R., Medlin, L. K., & Syvertsen, E. E. (1994). Synedropsis gen. nov., a genus of araphid diatoms associated with sea ice. Phycologia, 33(4), 248–270. https://doi.org/10.2216/i0031-8884-33-4-248.1

A new araphid diatom genus, Synedropsis Hasle, Medlin et Syvertsen, is described from sea ice. The generitype, Synedropsis hyperborea (Grunow) Hasle, Medlin et Syvertsen from the Arctic, was first described as a species of Synedra, as was the antarctic Synedropsis fragilis (Manguin) Hasle, Syvertsen et Medlin. A second antarctic species of Synedropsis is a new combination of Cymatosira laevis Heiden in Heiden & Kolbe. In addition four new taxa, S. hyperboreoides Hasle, Syvertsen et Medlin, S. recta Hasle, Medlin et Syvertsen, S. lata Hasle, Medlin et Syvertsen and S. lata var. angustata Hasle, Medlin et Syvertsen are described from the Antarctic. The valve wall is laminar with uniseriate, often poorly developed striae and a wide sternum. Each valve possesses apical fields composed of slits. A labiate process is positioned near one apical slit field. The valve outline for most species exhibits considerable stadial variation. The girdle has several bands, most with one row of poroids close to the pars interior. Thus Synedropsis is closely related to the marine Fragilaria striatula Lyngbye except in the structure of the apical fields and the number of bands. Species observed in uncleaned material appeared in stellate or, more seldom, ribbon-shaped colonies. Synedropsis hyperborea is a common epiphyte on the ice-associated Melosira arctica Dickie in the Arctic. The antarctic species were found mainly in the bottom ice community, S. fragilis as an epiphyte on other diatoms.

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Isaksson, E., & Karlén, W. (1994). High resolution climatic information from short firn cores, western Dronning Maud Land, Antarctica. Climatic Change, 26, 421–434. https://doi.org/10.1007/BF01094405

In this paper a detailed record of major ions from a 20 m deep firn core from Amundsenisen, western Dronning Maud Land, Antarctica, is presented. The core was drilled at 75° S, 2° E (2900 m a.s.l.) during austral summer 1991/92. The following ions were measured at 3 cm resolution: Na+, Mg2+, Ca2+, Cl−, NO3−, S04 2− and CH3SO3H (MSA). The core was dated back to 1865 using a combination of chemical records and volcanic reference horizons. The volcanic eruptions identified in this core are Mount Ngauruhoe, New Zealand (1974–75), Mount Agung, Indonesia (1963), Azul, Argentina (1932), and a broad peak that corresponds in time toTarawera, New Zealand (1886), Falcon Island, South Shetlands, Southern Ocean (1885), and Krakatau, Indonesia (1883). There are no trends in any of the ion records, but the annual to decadal changes are large. The mean concentrations of the measured ions are in agreement with those from other high-altitude cores from the Antarctic plateau. At this core site there may be a correspondence between peaks in the MSA record and major El Niño–Southern Oscillation events.
Isaksson, E., & Karlén, W. (1994). Spatial and temporal patterns in snow accumulation, western Dronning Maud Land, Antarctica. Journal of Glaciology, 40(135), 399–409. https://doi.org/10.3189/S0022143000007486

During the Swedish Antarctic Expedition to Dronning Maud Land, Antarctica, 1988–89 the net accumulation was estimated for an area from the coast to about 400 km inland. Stake measurements were used to obtain the spatial variability and firn cores were used for the temporal variability. The mean annual accumulation for the period 1976–88 is about 0.4mw.e. for Riiser-Larsenisen and about 0.3mw.e. for the area above the grounding line. The accumulation rate at higher altitudes, > 2500 m a.s.1., is about 0.1 m w.e. for 1955–88. One record from the ice shelf covers the period 1957–88, and suggests an increase in accumulation of about 12%. Between 1976 and 1988, the accumulation has decreased by about 50%, most likely due to lower temperatures as suggested by the temperature record from Halley.

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Joyner, C. C. (1994). The legitimacy of the Convention on the on the Regulation of Antarctic Mineral Resource Activities (p. 21). Fridtjof Nansens institutt.
Kagge, E. (1994). Alene til Sydpolen. Polarboken, 1993/94, 7–9.
Lorentsen, S.-H. (1994). Antarktis - den siste villmark. NINA-Nytt, 6–9.
Lorentsen, S.-H., & Røv, N. (1994). Sex determination of Antarctic Petrels Thalassoica antarctica by discriminant analysis of morphometric characters. Polar Biology, 14(2), 143–145. https://doi.org/10.1007/BF00234977

We present data on sexual dimorphism in some morphological measurements (wing length, head length, bill depth and bill length) in the Antarctic Petrel Thalassoica antarctica. Males were on average larger than females for all measurements. Sexual dimorphism was on average largest for bill depths whereas wing lengths discriminated least between the sexes. A discriminant function including bill depth, head length and wing length correctly sexed 92% of the sample. Due to between-measurer variation it is recommended that morphometric measurements obtained by others on sexed birds are compared with ours before proceeding with the use of the discriminant function on unsexed individuals.

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Mårtensson, P.-E., Nordøy, E. S., & Blix, A. S. (1994). Digestibility of krill (Euphausia superba and Thysanoessa sp.) in minke whales (Balaenoptera acutorostrata) and crabeater seals (Lobodon carcinophagus). British Journal of Nutrition, 72(5), 713–716. https://doi.org/10.1079/BJN19940073
Newton, I. P., Cooper, J., Mehlum, F., & Thor, G. (1994). A bibliography of terrestrial biological research in Dronning Maud Land, Antarctica. South African Journal of Antarctic Research, 24(1/2), 111–124.

A bibliography of terrestrial biological research in Dronning Maud Land, Antarctica, of 388 titles from 1954 to 1994 is provided as an aid to researchers working in the region.
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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Olsen, P. E. (1994). Hvalfangstens økonomiske betydning for Vestfold i mellomkrigstiden. P.E. Olsen.
Orrego Vicuña, F. (1994). The protocol on environmental protection to the Antarctic Treaty: the question of effectiveness (p. 14). Fridtjof Nansens institutt.
Østerhus, S. (ed. ). (1994). Report of the Norwegian Antarctic Research Expedition 1991/1992 (Vol. 124). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173020

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