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

Page 57 of 145

Abstracts

Skvarca, P., Rack, W., Rott, H., & Ibarzábal Donángelo, T. (1999). Climatic trend and the retreat and disintegration of ice shelves on the Antarctic Peninsula: an overview. Polar Research, 18(2), 151–157. https://doi.org/10.3402/polar.v18i2.6568

Observation of the retreat and disintegration of ice shelves around the Antarctic Peninsula during the last three decades and associated changes in air temperature, measured at various meteorological stations on the Antarctic Peninsula, are reviewed. The climatically induced retreat of the northern Larsen Ice Shelf on the east coast and of the Wordie, George VI, and Wilkins ice shelves on the west coast amounted to about 10 000 km2 since the mid-1960s. A summary is presented on the recession history of the Larsen Ice Shelf and on the collapse of those sections north of Robertson Island in early 1995. The area changes were derived from images of various satellites, dating back to a late 1963 image from the recently declassified US Argon space missions. This photograph reveals a previously unknown, minor advance of the northern Larsen Ice Shelf before 1975. During the period of retreat a consistent and pronounced warming trend was observed at the stations on both east and west coasts of the Antarctic Peninsula, but a major cause of the fast retreat and final collapse of the northernmost sections of the Larsen Ice Shelf were several unusually warm summers. Temperature records from the nearby station Marambio show that a positive mean summer temperature was reached for the first time in 1992-93. Recent observations indicate that the process of ice shelf disintegration is proceeding further south on both sides of the Antarctic Peninsula.

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Swithinbank, C. (1999). Foothold on Antarctica : the first international expedition (1949-1952) : through the eyes of its youngest member. Book Guild.
Tveraa, T. (ed. ), & Winther, J.-G. (ed. ). (1999). Report of the Norwegian Antarctic Research Expedition 1997/98 (Vol. 156). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173073

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Tveraa, T., Andreassen, C., & Christensen, G. N. (1999). Studies of seabirds at Svarthamaren. In T. (ed. ) Tveraa & J.-G. (ed. ) Winther (Eds.), Report of the Norwegian Antarctic Research Expedition 1997/98 (Vol. 156, pp. 26–29). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173073

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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.
van Franeker, J. A., Gavrilo, M., Mehlum, F., Veit, R. R., & Woehler, E. J. (1999). Distribution and Abundance of the Antarctic Petrel. Waterbirds: The International Journal of Waterbird Biology, 22(1), 14–28. https://doi.org/10.2307/1521989

Published and unpublished information on the distribution and abundance of the Antarctic Petrel (Thalassoica antarctica) is reviewed. Currently 35 colonies with approximately half a million breeding pairs are known. All but one of these known colonies are situated in East Antarctica. However, an estimate derived from at sea studies in three of four apparent centers of oceanic occurrence suggests a population as high as four to seven million breeding pairs (10 to 20 million individuals). In spite of the tentative nature of such an estimate, the difference with the colony-derived figure strongly suggests the existence of large, currently undiscovered colonies, particularly in western Antarctica and Victoria Land, where a complete mismatch exists between bird observations at sea and known colonies. In eastern Antarctica, in addition to undiscovered colonies, some known ones could be considerably larger than currently documented.

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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.
Young, O. R. (1999). The interplay of global and polar regimes. Polar Research, 18(2), 397–402. https://doi.org/10.3402/polar.v18i2.6601

The growing salience of interactions between the functionally broad but geographically narrow regimes for the polar regions and the geographically broad but functionally specific regimes emerging to deal with global environmental changes directs attention to the issue of institutional interplay. Interplay among regimes can cause mutual interference or foster synergy. Adopting a pragmatic stance that assumes no fundamental changes in international society, this essay suggests ways to: (1) adapt global regimes dealing with ozone depletion, climate change and biodiversity to the conditions prevailing in the polar regions; and (2) ensure that concerns arising in the polar regions receive serious consideration in global forums. Specific suggestions range from modest initiatives involving monitoring and assessment to more ambitious initiatives, such as the establishment of a chamber of regions in global regimes.

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Aldahan, A., Possnert, G., Johnsen, S. J., Clausen, H. B., Isaksson, E., Karlen, W., & Hansson, M. (1998). Sixty year 10Be record from Greenland and Antarctica. Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, 107(2), 139–147. https://doi.org/10.1007/BF02840464

We report in this study the distribution of 10Be in the top 40 m of the Renland ice core (East Greenland) and in a 30 m long core from DML (Dronning Maud Land, Antarctica) for the period 1931–1988. The two sites show differences in10Be content, the Antarctica site showing smaller variance and a lower average 10Be annual flux. Similarly, the average accumulation rate (cm water equivalent year−1) is higher in the Renland relative to DML. The variability in accumulation (precipitation) rates seems to explain part of the difference in10Be flux between the two polar sites. Cyclic fluctuations of 10Be flux correlate with the 11-year sunspot number and cosmic ray intensity than with the aa index (perturbation of the geomagnetic activity by the solar wind). Our data corroborate 10Be cyclic fluctuation pattern from the Dye 3 ice core and confirm a promising potential for correlation of global and local events.

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Amundsen, R. (1998). Dagboken fra Belgica-ekspedisjonen 1897-99 : Roald Amundsens første ferd til Antarktis (Vol. 3). Vågemot miniforl. https://doi.org/oai:nb.bibsys.no:999916658564702202 URN:NBN:no-nb_digibok_2010081608024

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Barker, P., Barrett, P., Camerlenghi, A., Cooper, A., Davey, F., Domack, E., Escutia, C., Kristoffersen, Y., & O’Brien, P. (1998). Ice sheet history from Antarctic Continental Margin sediments: The ANTOSTRAT approach. Terra Antarctica, 5(4), 737–760. http://pubs.er.usgs.gov/publication/70020442

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Barr, S. (1998). Polare jubileer i 1997 og 1998. Polarboken, 1997/98, 33–40.
Basberg, B. L. (1998). “Convergence or National Styles? The Japanese Challenge to the British-Norwegian Hegemony in the Twentieth-Century Whaling Industry.” In D. J. Starkey & G. Harlaftis (Eds.), Global Markets: The Internationalization of the Sea Transport Industries since 1850 (Vol. 14, pp. 259–284). Liverpool University Press. https://www.cambridge.org/core/books/global-markets/convergence-or-national-styles-the-japanese-challenge-to-the-britishnorwegian-hegemony-in-the-twentiethcentury-whaling-industry/AB128B6ED1F32F3466E03FC251FD27C6

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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.
Bomann-Larsen, T. (1998). Roald Amundsen : en biografi. Cappelen. https://doi.org/oai:nb.bibsys.no:999819559244702202 URN:NBN:no-nb_digibok_2008082100043

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Erikstad, K. E., Fauchald, P., Tveraa, T., & Steen, H. (1998). On the cost of reproduction in long-lived birds: the influence of environmental variability. Ecology, 79(5), 1781–1788. https://doi.org/https://doi.org/10.1890/0012-9658(1998)079[1781:OTCORI]2.0.CO;2

View on esajournals.onlinelibrary.wiley.com
fiskeridepartementet, N.- og. (1998). Forskrift om regulering av fiske med norske fartøyer i Antarktis (CCAMLR-området). Lovdata. https://lovdata.no/dokument/SF/forskrift/1998-03-13-195?q=antarktis

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Froneman, P. W., Pakhomov, E., Turner, D., Abrahamson, K., Karlsson, B., Godhe, A., Bertilsson, S., Graneli, W., Carlsson, P., Wängberg, S.-Å., Wulff, A., Croot, P., Andersson, K., Balarin, M., Wedborg, M., Persson, T., Rasmus, K., Ozturk, M., & David, R. (1998). Research cruise of the Scandinavian South African Antarctic expedition, December 1997 to February 1998. South African Journal of Science, 94(11), 517–519. http://hdl.handle.net/10962/d1011955

Focuses on the Scandinavian/South African Antarctic expedition conducted between December 4, 1997 to February 6, 1998 which determined the role of Southern Ocean in the global carbon cycle in physical and biological oceanographic studies. Aims of the expedition; Underway sampling conducted; Biological results of the expedition; Conclusions.

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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.

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