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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Publication year

Between 1900 and 1999
- Between 1990 and 1999
  - 1998

Results 45 resources

Abstracts

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

View on urn.nb.no
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

View on pubs.er.usgs.gov
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

View on urn.nb.no
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.
Hansson, R. (1998). Norvegija i poljarnye rajony. Izdano Ministerstvom inostrannych del Norvegii.
Hansson, R. (1998). Norway and the polar regions. The Royal Norwegian Ministry of Foreign Affairs. https://doi.org/oai:nb.bibsys.no:999815623024702202 URN:NBN:no-nb_digibok_2008121700033

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Hansson, R. (1998). Norwegen und die Polargebiete. Kgl. Norwegisches Ministerium für Auswärtige Angelegenheiten.
Hansson, R. (ed. ). (1998). Norge og polarområdene. Utenriksdepartementet. https://doi.org/oai:nb.bibsys.no:999815621914702202 URN:NBN:no-nb_digibok_2008111900044

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Haugland, J. E. (1998). Den norske antarktisekspedisjonen (NARE) 1996/97. Polarboken, 1997/98, 12–19.
Kallenborn, R., Oehme, M., Wynn-Williams, D. D., Schlabach, M., & Harris, J. (1998). Ambient air levels and atmospheric long-range transport of persistent organochlorines to Signy Island, Antarctica. Science of The Total Environment, 220(2), 167–180. https://doi.org/10.1016/S0048-9697(98)00257-5

Levels of persistent organic pollutants (POPs), such as polychlorinated biphenyls and pesticides have been determined in ambient air at Signy Island, Antarctica, over a period of 17 weeks. Mean concentrations for single polychlorinated biphenyls (0.02–17 pg/m3), for chlordanes (0.04–0.9 pg/m3), DDT compounds (0.07–0.40 pg/m3) and γ-hexachlorocyclohexane (HCH, 22 pg/m3) were comparable to those in Arctic air. However, α-HCH levels were approximately one order of magnitude lower. Compared to the Arctic, differences were also observed in the concentration ratios of α-/γ-HCH and chlordane compounds. Two possible atmospheric long-range transport episodes from South America were found by comparing 10-day back trajectories with observed concentration changes. The lower limits of determination (LOD) were mainly governed by the field blanks. They were satisfactory for the most volatile PCBs. However, many concentrations for DDT and chlordane compounds were below the LODs (range 0.1–1 pg/m3) or even the instrumental detection limit (0.01–0.03 pg/m3).

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Kristiansen, S., Farbrot, T., Kuosa, H., Myklestad, S. M., & Quillfeldt von, C. H. (1998). Nitrogen uptake in the infiltration community, an ice algal community in Antarctic pack-ice. Polar Biology, 19(5), 307–315. https://doi.org/10.1007/s003000050251

An infiltration community was the dominating ice algal community in pack-ice off Queen Maud Land, Southern Ocean, in January 1993. The community was dominated by autotrophic processes, and the most common species were the prymnesiophyte Phaeocystis antarctica and the diatoms Chaetoceros neglectus and Fragilariopsis cylindrus. The concentration of chlorophyll a was 1.3–47.9 μg l−1, and the inner part of the community was nitrate depleted. Uptake rates of nitrate, nitrite, ammonium, urea and amino acids were measured using 15N. Nitrate was the major nitrogen source for ice algal growth (67 ± 6% nitrate uptake). It is suggested that % nitrate uptake in the infiltration community decreases during the growth season, from 92% during spring (literature data) to 67% during summer. Scalar irradiance in the infiltration community was high and variable. It reached ca. 2000 μmol m−2 s−1 at some locations, and nitrate uptake rate was potentially photoinhibited at irradiances >500 μmol m−2 s−1. Nitrate uptake rate in an average infiltration community (0.6 m of snow cover) was lowered by 13% over a 2-week period due to photoinhibition.

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Licht, K. J., Cunningham, W. L., Andrews, J. T., Domack, E. W., & Jennings, A. E. (1998). Establishing chronologies from acid-insoluble organic 14C dates on Antarctic (Ross Sea) and Arctic (North Atlantic) marine sediments. Polar Research, 17(2), 203–216. https://doi.org/10.3402/polar.v17i2.6619

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