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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Between 1900 and 1999

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Results 856 resources

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Abstracts

Amundsen, R., & Decleir, H. (Red. ). (1999). Roald Amundsen’s Belgica diary : the first scientific expedition to the Antarctic. Bluntisham Books.
Eiken, T., Omang, O. C. D., & Øvstedal, O. (1999). A local geoid in Dronning Maud Land. 24th General Assembly European Geophysical Society.

The main purpose of the present paper is to estimate the orthometric height of the GPS-station at Troll, Dronning Maud Land, Antarctica. Located at approximately 1300 m Troll has been connected to the GIANT-network, but it's orthometric height remains undetermined. A local geoid has been determined based on available gravity anomalies and vertical angle mesurements. Information about the ice-thickness has been included in the terrain model. Based on tidal measurements the mean sea level was determined in Jutulgryta, a rift zone in the Fimbulisen ice shelf. Several gravity- and GPS-stations were measured between the two points (Jutulgryta and Troll), a distance of approximately 100 km.
Glines, C. V. (1999). Bernt Balchen : polar aviator. Smithsonian Institution Press.
Honda, K. (1999). Scott and Amundsen (Vol. 28). The Asahi-Shinbun.
Jenssen, H. L. (1999). Den første olje. In Ambra : Sandefjordmuseene årbok (Vol. 1999, pp. 11–24). Sandefjordmuseene.
Killie, B., Savinova, T., Kleivane, L., Lie, E., Skaare, J. U., & Nygård, T. (1999). Antarktis. In J. Knutzen (Ed.), Miljøgifter og radioktivitet i norsk fauna: inkludert Arktis og Antarktis (Vols. 1999–5, pp. 189–196). Direktoratet for naturforvaltning.
Klages, N., Hofmeyr, G., & Gjertz, I. (1999). Prey of Antarctic fur seals at Bouvetøya, Southern Ocean. Polar Record, 35(194), 255–257. https://doi.org/10.1017/S0032247400015527
Knutzen, J., Fjeld, E., Hylland, K., Killie, B., Kleivane, L., Lie, E., Nygård, T., Savinova, T., Skåre, J. U., & Aanes, K. J. (1999). Miljøgifter og radioaktivitet i norsk fauna : inkludert Arktis og Antarktis (J. Knutzen, Ed.; Vols. 1999–5). Direktoratet for naturforvaltning.
Lie, E., Nygård, T., Røv, N., & Steinnes, E. (1999). Akkumulering av tungmetaller i en antarktisk næringskjede. In T. Nygård & B. Jonsson (Eds.), NINAs strategiske instituttprogrammer 1991-95. Forurensningsøkologi. Sluttrapport (Vol. 10, pp. 66–70). Norsk institutt for naturforskning.
Liston, G. E., Winther, J.-G., Bruland, O., Elverhøy, H., & Sand, K. (1999). Below-surface ice melt on the coastal Antarctic ice sheet. Journal of Glaciology, 45(150), 273–285. https://doi.org/10.3189/S0022143000001775

In the Jutulgryta area of Dronning Maud Land, Antarctica, subsurface melting of the ice sheet has been observed. The melting takes place during the summer months in blue-ice areas under conditions of below-freezing air and surface temperatures. Adjacent snow-covered regions, having the same meteorological and climatic conditions, experience little or no subsurface melting. To help explain and understand the observed melt-rate differences in the blue-ice and snow-covered areas, a physically based numerical model of the coupled atmosphere, radiation, snow and blue-ice system has been developed. The model comprises a heat-transfer equation which includes a spectrally dependent solar-radiation source term. The penetration of radiation into the snow and blue ice depends on the solar-radiation spectrum, the surface albedo and the snow and blue-ice grain-sizes and densities. In addition, the model uses a complete surface energy balance to define the surface boundary conditions. It is run over the full annual cycle, simulating temperature profiles and melting and freezing quantities throughout the summer and winter seasons. The model is driven and validated using field observations collected during the Norwegian Antarctic Research Expedition (NARE) 1996–97. The simulations suggest that the observed differences between subsurface snow and blue-ice melting can be explained largely by radiative and heat-transfer interactions resulting from differences in albedo, grain-size and density between the two mediums.
Melvold, K. (1999). Impact of recent climate on glacier mass balance : studies on Kongsvegen, Svalbard and Jutulstraumen, Antarctica. University of Oslo.
Swithinbank, C. (1999). Foothold on Antarctica : the first international expedition (1949-1952) : through the eyes of its youngest member. Book Guild.
van den Broeke, M. R., Winther, J.-G., Isaksson, E., Pinglot, J. F., Karlöf, L., Eiken, T., & Louk, C. (1999). Climate variables along a traverse line in Dronning Maud Land, East Antarctica. Journal of Glaciology, 45(150), 295–302. https://doi.org/10.3189/S0022143000001799

Temperature, density and accumulation data were obtained from shallow firn cores, drilled during an overland traverse through a previously unknown part of Dronning Maud Land, East Antarctica. The traverse area is characterised by high mountains that obstruct the ice flow, resulting in a sudden transition from the polar plateau to the coastal region. The spatial variations of potential temperature, near-surface firn density and accumulation suggest that katabatic winds are active in this region. Proxy wind data derived from firn-density profiles confirm that annual mean wind speed is strongly related to the magnitude of the surface slope. The high elevation of the ice sheet south of the mountains makes for a dry, cold climate, in which mass loss owing to sublimation is small and erosion of snow by the wind has a potentially large impact on the surface mass balance. A simple katabatic-wind model is used to explain the variations of accumulation along the traverse line in terms of divergence/convergence of the local transport of drifting snow. The resulting wind- and snowdrift patterns are closely connected to the topography of the ice sheet: ridges are especially sensitive to erosion, while ice streams and other depressions act as collectors of drifting snow.
Vidas, D. (1999). The Southern Ocean seabed: arena for conflicting regimes? In D. Vidas & W. Østreng (Eds.), Order for the oceans at the turn of the century (pp. 291–314). Kluwer.
Barr, S. (1998). Polare jubileer i 1997 og 1998. Polarboken, 1997/98, 33–40.
Basberg, B. L. (1998). The Floating Factory: Dominant Designs and Technological Development of Twentieth-CenturyWhaling Factory Ships. The Northern Mariner/Le Marin Du Nord, VIII(1), 21–37.
Hamran, S. E., Erlingsson, B., Gjessing, Y., & Mo, P. (1998). Estimate of the subglacier dielectric constant of an ice shelf using a ground-penetrating step-frequency radar. IEEE Transactions on Geoscience and Remote Sensing, 36(2), 518–525. https://doi.org/10.1109/36.662734

The mass balance of the Antarctic ice cap, its stability, and the role of the surrounding ice shelf in bottomwater mass formation is, to a large extent, dictated by processes associated with subsurface freezing and melting, where the submerged ice meets the surrounding ocean. It is demonstrated how multifrequency ground-penetrating radar data collected at the Riiser-Larsenisen can be used to examine the physical conditions of the ice-shelf subsurface. The received radar signal from three different frequency intervals, 10-30, 155-170, and 330-360 MHz (range of wavelengths from 15 to 0.5 m in the ice), was analyzed by using a plane reflector model. It is demonstrated that the data can be successfully used to distinguish between types of ice at the ice-ocean interface, such as for freezing marine ice, melting marine ice, melting meteoric ice from the ice cap, and melting firn/ice. The data analysis shows that the subsurface can be regarded as rough on length scales in the order of 1 m.
Hansson, R. (1998). Noruega y las regiones polares. Real Ministerio Noruego de Asuntos Exteriores.
Hansson, R. (1998). Norvegija i poljarnye rajony. Izdano Ministerstvom inostrannych del Norvegii.
Hansson, R. (1998). Norwegen und die Polargebiete. Kgl. Norwegisches Ministerium für Auswärtige Angelegenheiten.

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