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

Foldvik, A., & Gammelsrød, T. (1988). Notes on Southern Ocean hydrography, sea-ice and bottom water formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 67(1), 3–17. https://doi.org/https://doi.org/10.1016/0031-0182(88)90119-8

The Southern Ocean circulation and sea-ice distribution is briefly described. The formation of extremely cold bottom water in the Weddell Sea and its relation to the floating Ronne-Filchner Ice Shelves is discussed. It is shown that a concentrated swift eroding bottom current with anomalous low ratio transports the cold and dense ice Shelf Water from the shelf towards large depths. Comments are made on possible implications of this process for the large-scale deep-water circulation and for the interpretation of sediment cores.

View on www.sciencedirect.com
Haftorn, S., Mehlum, F., & Bech, C. (1988). Navigation to nest site in the snow petrel (Pagodroma nivea). The Condor, 90(2), 484–486. https://doi.org/10.2307/1368578

View on www.jstor.org
Haftorn, S., Mehlum, F., & Bech, C. (1988). Size variation in the snow petrel Pagodroma nivea. Notornis, 35(2), 109–116.
Horner, R. A., Syvertsen, E. E., Thomas, D. P., & Lange, C. (1988). Proposed terminology and reporting units for sea ice algal assemblages. Polar Biology, 8(4), 249–253. https://doi.org/10.1007/BF00263173

View on doi.org
Huntford, R., & Hoff, T. (1988). Sydpolen 1910-1912. In Roald Amundsens oppdagelsesreiser i bilder (pp. 39–142, ill.). Grøndahl. https://doi.org/oai:nb.bibsys.no:998830791604702202 URN:NBN:no-nb_digibok_2013091638079

View on urn.nb.no
Jakobsen, Ø., & Fiskeridirektoratet. (1988). Skjellressurser i Sydishavet: litteraturstudie (p. 29). Norges fiskerihøyskole. http://hdl.handle.net/11250/131092

View on hdl.handle.net
Koren, J. (1988). Journal over den Belgiske Sydhavs-Expedition 97-99. https://media.digitalarkivet.no/view/77494/59

View on media.digitalarkivet.no
Kristensen, M. (1988). Mot 90⁰ syd, en rapport. Polarboken, 1987/88, 23–28.
Kristoffersen, Y., & Aalerud, J. (1988). Aeromagnetic reconnaissance over the Riiser-Larsen Ice Shelf, east Antarctica. Polar Research, 6(1), 123–128. https://doi.org/10.3402/polar.v6i1.6852

View on polarresearch.net
Larsen, H.-K. (1988). Minnesmerket på Østre Halsen over antarktispioneren C.A. Larsen. Polarboken, 1987/88, 11–13.
Løvlie, R. (1988). Evidence for deuteric magnetization in hydrothermally altered Mesozoic basaltic rocks from East Antarctica. Physics of the Earth and Planetary Interiors, 52(3/4), 352–364. https://doi.org/10.1016/0031-9201(88)90127-6

Mesozoic basaltic lavas and dykes from Vestfjella, East Antarctica, are dominated by well-grouped, single-component palaeomagnetic directions of normal polarity. Reversed magnetizations, heavily overprinted by normal polarity components, were encountered in a few lava flows and dykes. Only thermal demagnetization was successful in separating tight distributions of reversed polarity directions, interpreted to represent a deuteric magnetization. The region has been exposed to regional hydrothermal alteration to the epidote/prehnite metamorphic facies (T ≈ 300°C). Titanomagnetite grains in high-temperature oxidation classes II–III show alteration features typical for hydrothermally altered basalts; partial to complete replacement of both ilmenite and magnetite to sphene is common in the most altered rocks, which also exhibit varying degrees of decomposition of the opaque minerals. The lavas display two major, but distinctly different, thermomagnetic curves; the ‘kink’ type, previously reported from rocks exposed to the epidote metamorphic facies, and curves dominated by a paramagnetic contribution defining a magnetite Curie point. It is concluded that the basalts have retained palaeomagnetic directions acquired during the deuteric cooling phase, implying that granulation/sphene formation and Fe depletion of decomposed titanomagnetite grains in classes II–III do not necessarily cause complete remagnetization or the acquisition of significant secondary remanent magnetizations.
Mehlum, F., Gjessing, Y., Haftorn, S., & Bech, C. (1988). Census of breeding Antarctic petrels Thalassoica antarctica and physical features of the breeding colony at Svarthamaren, Dronning Maud Land, with notes on breeding snow petrels Pagodroma nivea and south polar skuas Catharacta maccormicki. Polar Research, 6(1), 1–9. https://doi.org/10.3402/polar.v6i1.6841

View on doi.org
Orheim, O. (1988). Antarctic icebergs: production, distribution and disintegration (abstract). Annals of Glaciology, 11, 205. https://doi.org/10.3189/S0260305500006649

A programme of systematic iceberg observations was initiated in 1981 by Norsk Polarinstitutt through the SCAR Working Group on Glaciology. Icebergs are recorded every 6 h and in five length groups: 10-50, 50-200, 200-500 and 500-1000 m, and those over 1000 m, which are described individually. Data on more than 100 000 icebergs are now on file at Norsk Polarinstitutt, and practically all ships travelling to and from Antarctica participate in the collection of data. This paper presents the first comprehensive analysis of the iceberg data. The quality of the data set is discussed, with consideration of potential errors in and limitations of the data, and various statistical evaluations. Representative distribution data are presented, and used to determine iceberg production, disintegration and mean residence times, and regional and total Antarctic calving rates. The incidence of large-scale calving in particular is evaluated, including the remarkably large break-offs in recent years. These exceed both the total annual accumulation on the Antarctic continent and the mean annual calving rate as determined from ship observations. The results show further: (1) that there are more than 200 000 icebergs south of the Antarctic Convergence, (2) that there are large regional differences in iceberg calving rates and iceberg sizes, and (3) that the calving rate from Antarctica is higher than that given in most previous estimates, which implies (4) that the mass balance of the Antarctic ice sheet is not positive as suggested by most recent estimates.

View on www.cambridge.org
Orheim, O., & Lucchitta, B. K. (1988). Numerical Analysis of Landsat Thematic Mapper Images of Antarctica: Surface Temperatures and Physical Properties. Annals of Glaciology, 11, 109–120. https://doi.org/10.3189/S026030550000642X

View on www.cambridge.org
Øvstedal, D. O. (1988). Cladonia galindezii, a new Antarctic lichen species. Cryptogamie, Bryologieet Lichénologie, 9, 137–139.
Øvstedal, D. O. (1988). On the variation of Ochrolechia parella in the western Antarctic and Subantarctic area. Polarforschung, 58(2), 77–82.
[Smedvig, N. (1988). Belgica : den første overvintringen i Antarktis 1897-1899. [Nordsjøselskapet]. https://doi.org/oai:nb.bibsys.no:990702483464702202 URN:NBN:no-nb_digibok_2009103004042

View on urn.nb.no
Sollie, F. (1988). The legitimacy of concluding an Antarctic mineral resources convention among the Atarctic Treaty parties. In R. Wolfrum (Ed.), Antarctic challenge III: conflicting interests, cooperation, environmental protection, economic development (Vol. 105, pp. 297–307). Duncker & Humblot.
Svendsen, K., & Eiken, T. (1988). Ekspedisjonen til Peter I Øy. Polarboken, 1987/88, 14–22.
Wójcik, G. (1988). Temperature of active layer at Bunger Oasis in Antarctica in summer 1978-79. In K. Sennest (Ed.), Proceedings / Permafrost, Fifth International Conference (Vol. 1, pp. 505–510). Tapir.

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Last update from database: 11/1/24, 3:10 AM (UTC)

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