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 2000 and 2025
- Between 2000 and 2009
  - 2006

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Results 15 resources

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Ackley, S., & Worby, T. (2006). Antarctic sea ice processes and climate program, The International Polar Year. Ice and Climate News, 7, 12.
Barbante, C. (2006). One-to-one coupling of glacial climate variability in Greenland and Antarctica. Nature, 444, 195–198. https://doi.org/10.1038/nature05301

Precise knowledge of the phase relationship between climate changes in the two hemispheres is a key for understanding the Earth’s climate dynamics. For the last glacial period, ice core studies1,2 have revealed strong coupling of the largest millennial-scale warm events in Antarctica with the longest Dansgaard–Oeschger events in Greenland3,4,5 through the Atlantic meridional overturning circulation6,7,8. It has been unclear, however, whether the shorter Dansgaard–Oeschger events have counterparts in the shorter and less prominent Antarctic temperature variations, and whether these events are linked by the same mechanism. Here we present a glacial climate record derived from an ice core from Dronning Maud Land, Antarctica, which represents South Atlantic climate at a resolution comparable with the Greenland ice core records. After methane synchronization with an ice core from North Greenland9, the oxygen isotope record from the Dronning Maud Land ice core shows a one-to-one coupling between all Antarctic warm events and Greenland Dansgaard–Oeschger events by the bipolar seesaw6. The amplitude of the Antarctic warm events is found to be linearly dependent on the duration of the concurrent stadial in the North, suggesting that they all result from a similar reduction in the meridional overturning circulation.
Basberg, B. L. (2006). In the wake of Tønnessen and Johnsen : trends in whaling history research after 1970. In J. E. Ringstad (Ed.), Whaling and History II : new perspectives (Vol. 31, pp. 11–21). Sandefjordmuseene.

In 1970 the fourth and final volume of Arne Odd Johnsen and Joh. N. Tønnessens’s Den moderne hvalfangsts historie was published. The work represented a milestone in the writing about the development of the 20th century whaling industry. This paper reviews the literature that has been published in Norway and internationally on the history of modern whaling after Johnsen and Tønnessen, and analyses the focus, trends and direction in the research and writing on whaling history in the period.
Børresen, D. I. (2006). The black book of 1913 - a means of disciplining whaling employees. In J. E. Ringstad (Ed.), Whaling and History II : new perspectives (Vol. 31, pp. 39–48). Sandefjordmuseene.
Haas, C. (2006). the Antarctic buoy program faces new challenges. Ice and Climate News, 7, 10–11.
Headland, R. K. (2006). Whalers and explorers; logistic assistance provided to people whose work, and indeed survival, depended on the whalers. In J. E. Ringstad (Ed.), Whaling and History II : new perspectives (Vol. 31, pp. 49–55). Sandefjordmuseene.
Lockyer, C. (2006). Cetacean feeding, growth and energetics in relation to the marine ecosystem - implications for management? In J. E. Ringstad (Ed.), Whaling and History II : new perspectives (Vol. 31, pp. 101–111). Sandefjordmuseene.
Martinsen, J. R. (2006). Tilbake til Dronning Maud Land, 45 år etter. Polarboken, 2005/06, 18–22.
Michelet, J. (2006). Høyt mot nord, langt mot sør : reisebrev per satelitt fra Arktis og Antarktis. Oktober.
Monaghan, A. J., Bromwich, D. H., Fogt, R. L., Wang, S.-H., Mayewski, P. A., Dixon, D. A., Ekaykin, A., Frezzotti, M., Ian Goodwin, I., Isaksson, E., Kaspari, S. D., Morgan, V. I., Oerter, H., Van Ommen, T. D., Van der Veen, C. J., & Wen, J. (2006). Insignificant change in Antarctic snowfall since the International Geophysical Year. Science, 313(5788), 827–831. https://doi.org/10.1126/science.1128243
Ringstad, J. E. (2006). Bjarne Aagaard and his Crusade against Pelagic Whaling in the late 1920s. In J. E. Ringstad (Ed.), Whaling and History II : new perspectives (Vol. 31, pp. 167–178). Sandefjordmuseene.
Sefland, M. (2006). “Brategg” og ekspedisjonen til Antarktis i 1947/48: om skuta, ekspedisjonen og deltakrane. Isflaket, 8(3), 3–20.
Skog, C., & Sandberg, S. (2006). Sydpolen. In Cecilie Skog og de tre polene (pp. 92–127). Wigestrand.
Stepanjants, S. D., Cortese, G., Kruglikova, S. B., & Bjørklund, K. R. (2006). A review of bipolarity concepts: history and examples from Radiolaria and Medusozoa (Cnidaria). Marine Biology Research, 2(3), 200–241. https://doi.org/10.1080/17451000600781767

Bipolarity, its history and general interpretation are investigated and discussed herein. Apart from the classical view, namely that a bipolar distribution is a peculiar biogeographical phenomenon, we propose that it is ecologically controlled too. This approach was used for bipolarity assessment within the following groups: Phaeodaria, Nassellaria, Spumellaria (Radiolaria) and Medusozoa (Cnidaria). We recognize 46 bipolar radiolarian species and three radiolarian genera. However, although species concepts in radiolarians are relatively stable and well known, the high-rank taxonomy of radiolarians is still not well defined. Caution should therefore be taken in the interpretation of distribution data at a taxonomic level higher than the species. In the Medusozoa, bipolarity is observed for 23 species and 32 genera. The different ways in which bipolarity can develop are discussed under the different groups, but preference has been given to the recent and most probable routes of migration. In our investigation of the bipolarity phenomenon, we reviewed more than 400 articles dealing with taxonomy, ecology and biogeography of the modern fauna in both groups.
Winther, J.-G. (2006). Åpning av overvintringsstasjonen Troll. Polarboken, 2005/06, 11–17.

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Last update from database: 12/1/25, 3:10 AM (UTC)

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