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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Abstracts

Skog, C., & Sandberg, S. (2011). Antarktis : 71 dager, 1800 kilometer og én million tanker. Gyldendal.
Strand, K. O., Østerhus, S., & Gammelsrød, T. (2011). Overvåking av havklima i Antarktis. Klima : norsk magasin for klimaforskning, 6, 22–23.
Thuesen, N. P. (2011). Amundsens omstridte forløper ; Innsjøen under isen. Vi menn vitenskap & historie, 2, 18–21.
Winther, J.-G., & Coulthard, A. (2011). Clues to historical climate variation and future changes in sea level buried in the Antarctic ice (TASTE-IDEA). In O. Orheim & K. Ulstein (Eds.), International Polar Year 2007-2008 : the Norwegian contribution (pp. 88–92). Research Council of Norway.
Amundsen, R. (2010). Sydpolsekspedisjonen 1910-1912 (G. O. Kløver, Ed.). Frammuseet.
Amundsen, R. (2010). The South Pole expedition 1910-1912 (G. O. Kløver, Ed.). Frammuseet.
Amundsen, R., Diesen, J. A., & Lund, H. Ø. (2010). Roald Amundsens sydpolsferd (1910-1912) = Roald Amundsen’s South Pole expedition (1910-1912). Norsk filminstitutt.
Amundsen, R., Scott, R. F., Bjaaland, O., & Huntford, R. (2010). Race for the South Pole : the expedition diaries of Scott and Amundsen. Continuum.
Anschütz, H., & Isaksson, E. (2010). Mindre snø enn forventet i Antarktis. Klima: norsk magasin for klimaforskning, 19(4), 16–17.
Anschütz, H., Isaksson, E., Müller, K., Winther, J.-G., & Albert, M. (2010). East Antarctic snow accumulation changes. Ice and Climate News, 14, 12–13.
Biuw, M., Lydersen, C., Nico de Bruyn, P. J., Arriola, A., Hofmeyr, G. G. J., Kritzinger, P., & Kovacs, K. M. (2010). Long-range migration of a chinstrap penguin from Bouvetøya to Montagu Island, South Sandwich Islands. Antarctic Science, 22(2), 157–162. https://doi.org/10.1017/S0954102009990605

We describe a long-range migration of a pre-moulting adult chinstrap penguin from Bouvetøya, a small relatively recently established colony, to the South Sandwich Islands, where large, established colonies of this species reside. The trip lasted around three weeks, covered ∼3600 km, and the time of arrival was consistent with the annual moult. The bird did not travel along the shortest path or along a constant bearing, but instead followed what appeared to be a series of two or three rhumb lines of constant bearing. Small southward and northward deviations from the general path were consistent with local water currents. Travel speeds were high during daylight but decreased at night, suggesting that resting or opportunistic feeding occurred preferentially at night. While long-range winter migrations of chinstraps to feeding areas in the vicinity of distant colonies have been previously described, this is the first observation of such a trip during the period between breeding and moulting, and the first record of an individual actually arriving at one of these distant colonies. This has implications for understanding population structure and management of this important Southern Ocean predator.
Biuw, M., Nøst, O. A., Stien, A., Zhou, Q., Lydersen, C., & Kovacs, K. M. (2010). Effects of hydrographic variability on the spatial, seasonal and diel diving patterns of southern elephant seals in the eastern Weddell Sea. PloS One, 5(11), e13816. https://doi.org/10.1371/journal.pone.0013816

Weddell Sea hydrography and circulation is driven by influx of Circumpolar Deep Water (CDW) from the Antarctic Circumpolar Current (ACC) at its eastern margin. Entrainment and upwelling of this high-nutrient, oxygen-depleted water mass within the Weddell Gyre also supports the mesopelagic ecosystem within the gyre and the rich benthic community along the Antarctic shelf. We used Conductivity-Temperature-Depth Satellite Relay Data Loggers (CTD-SRDLs) to examine the importance of hydrographic variability, ice cover and season on the movements and diving behavior of southern elephant seals in the eastern Weddell Sea region during their overwinter feeding trips from Bouvetøya. We developed a model describing diving depth as a function of local time of day to account for diel variation in diving behavior. Seals feeding in pelagic ice-free waters during the summer months displayed clear diel variation, with daytime dives reaching 500-1500 m and night-time targeting of the subsurface temperature and salinity maxima characteristic of CDW around 150-300 meters. This pattern was especially clear in the Weddell Cold and Warm Regimes within the gyre, occurred in the ACC, but was absent at the Dronning Maud Land shelf region where seals fed benthically. Diel variation was almost absent in pelagic feeding areas covered by winter sea ice, where seals targeted deep layers around 500-700 meters. Thus, elephant seals appear to switch between feeding strategies when moving between oceanic regimes or in response to seasonal environmental conditions. While they are on the shelf, they exploit the locally-rich benthic ecosystem, while diel patterns in pelagic waters in summer are probably a response to strong vertical migration patterns within the copepod-based pelagic food web. Behavioral flexibility that permits such switching between different feeding strategies may have important consequences regarding the potential for southern elephant seals to adapt to variability or systematic changes in their environment resulting from climate change.
Divine, D., Koç, N., Isaksson, E., Nielsen, S. H., Crosta, X., & Godtliebsen, F. (2010). Holocene Antarctic climate variability from ice and marine sediment cores: insights on ocean-atmosphere interaction. Quaternary Science Reviews, 29(1/2), 303–312. https://doi.org/10.1016/j.quascirev.2009.11.012

Holocene climate variability in the southeast Atlantic sector of the Southern Ocean and Antarctic is assessed and quantified through integration of available marine sediment core and Antarctic ice core data. We use summer sea surface temperature (SSST) and sea ice presence (SIP) reconstructions from two marine sediment cores recovered north (50 °S) and south (53.2 °S) of the present day Antarctic Polar Front (APF), as well as an atmospheric temperature and sea ice proxy from the EPICA ice core from Dronning Maud Land (EDML). We find reasonably good agreement in the timing of climate evolution in the analyzed series. Almost all records show a gradual glacial-to-Holocene climate transition, interrupted by the Antarctic cold reversal around 13 000 cal yr BP, and early Holocene climatic optimum (HCO) at about 11 000 cal yr BP. During the early HCO, the seasonal ice cover retreats to south of 53 °S; it then readvances in the course of the mid- to late Holocene. The maximum winter sea ice edge position during the recent 10 000 years varied mainly within 51–53 °S, with sporadic growth to north of 50 °S, a position similar to that during the last glacial. The onset of the Neoglacial period after ca 4000 yr BP is associated with a steepening of the SSST gradient between the marine core sites, strengthening of the westerlies and cooling in the inland ice sheet. The agreement in timing between elevated SSST during the early HCO and decreased deuterium excess in EDML and other ice cores from different locations in the East Antarctic suggests that the retreat of sea ice during the early HCO and weakening of the APF was a general feature of the East Antarctic climate during that time.
Eisen, O., Hofstede, C., Miller, H., Kristoffersen, Y., Blenkner, R., Lambrecht, A., & Mayer, C. (2010). A New Approach for Exploring Ice Sheets and Sub-Ice Geology. Eos Transactions American Geophysical Union, 91(46), 429–430. https://doi.org/10.1029/2010EO460001
Fujise, Y., Hatanaka, H., & Ohsumi, S. (2010). Hva skjedde med vågehvalen i Antarktis? Ottar, 280 = 2010:2, 29–35.

Jakten på de store bardehvalene i antarktiske farvann startet på begynnelsen av 1900-tallet og reduserte bestandene sterkt. Vågehvalen ble mindre utsatt for fangst og fikk kanskje en fordel da de større konkurrentene forsvant? Det japanske forskningsprogrammet JARPA har studert endringer i det marine økosystemet i Antarktis.
Garmel, H. (2010). Whalers’ wives in Vestfold, Norway during the pelagic period. In J. E. Ringstad (Ed.), Whaling and History III : papers presented at a symposium in Sandefjord on the 18th and 19th of June 2009 (Vol. 33, pp. 161–168). Vestfoldmuseene IKS, avd. Hvalfangstmuseet.
Goldberg, F. (2010). Polarskipet Antarctics stolte historie. Del 2. Polarboken, 2009/10, 86–101.
Hofmeyr, G., Bester, M., Kirkman, S., Lydersen, C., & Kovacs, K. (2010). Intraspecific differences in the diet of Antarctic fur seals at Nyrøysa, Bouvetøya. Polar Biology, 33, 1–17. https://doi.org/10.1007/s00300-010-0805-0

Intraspecific differences in the diets of many species of pinnipeds are to be expected in view of the great differences in morphology, life history and foraging behaviour between the sexes of many species. We examined the diet of the Antarctic fur seal population at Bouvetoya, Southern Ocean, to assess intersexual differences. This was made possible by the analysis of prey remains extracted from scats and regurgitations collected in areas used primarily by one or the other sex. The results indicate that both males and females feed primarily on Antarctic krill Euphausia superba with several species of fish and squid being taken, likely opportunistically given their prevalence. Significant differences were identified in the frequency of occurrence of otoliths in scats and the percentage numerical abundance of the major fish prey species in the diet. Adult males ate a smaller quantity of fish overall, but ate significantly more of the larger fish species. The greater diving capabilities of males and the fact that they are not limited in the extent of their foraging area by having to return regularly to feed dependant offspring may play a role in the differences found between the diets of males and females. Additionally, females might be more selective, favouring myctophids because they are richer in energy than krill. The absence of major differences in the diet between the sexes at this location is likely due to the high overall abundance of prey at Bouvetoya.
Iversen, S. A. (Red. ), Myklevoll, S. (Red. ), Mæstad, K. (Red. ), & Nøttestad, L. (Red. ). (2010). Cruising for krill in the Southern Ocean with G.O. Sars. Institute of Marine Research.
Kløver, G. O. (Red. ). (2010). Antarctic pioneers : the voyage of the Belgica 1879-99. The Fram Museum.

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