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

Matsuoka, K. (ed. ). (2020). Life of the Antarctic ice : from deep inland to the coast. Norwegian Polar Institute.
Winther, J.-G. (2008). Klimagåten Antarktis. Gyldendal.
Melvold, K. (1999). Impact of recent climate on glacier mass balance : studies on Kongsvegen, Svalbard and Jutulstraumen, Antarctica. University of Oslo.
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.
Orheim, O. (1985). Iceberg discharge and the mass balance of Antarctica. National Academy Press.
Kristensen, M., & Squire, V. A. (1983). Automatic collection of tilt and strain data from tabular icebergs. Annals of Glaciology, 4, 147–151. https://doi.org/10.3189/S0260305500005383
Kristensen, M., & Squire, V. A. (1983). Modelling of antarctic tabular icebergs in ocean waves. Annals of Glaciology, 4, 152–157. https://doi.org/10.3189/S0260305500005395

The prediction of the motions of a tabular iceberg in a seaway is a problem which cannot be solved with a simple approach. The main difficulty lies in the size and mass of the iceberg, which produce frequency-dependent hydrodynamical effects as it moves in the water. Specifically, any solution must take into account both the added inertia and the generation of surface waves caused by the motions of the berg. Early attempts at modelling, which did not include these terms, could not accurately predict the complicated response behaviour seen in field data. In this paper we discuss some modifications to a two-dimensional simulation of floating bodies in waves, which must be applied when the motions and the hydro-dynamical pressures beneath tabular icebergs are required.
Orheim, O., & Govorukha, L. S. (1982). Present-day glaciation in the South Shetland Islands. Annals of Glaciology, 3, 233–238. https://doi.org/10.3189/S0260305500002834
Foldvik, A., Gammelsrød, T., & Gjessing, Y. (1980). Measurements of oscillations and flexure of icebergs. Annals of Glaciology, 1, 29–30. https://doi.org/10.3189/S0260305500016918
Foldvik, A., Gammelsrød, T., & Gjessing, Y. (1980). Measurements of the radiation temperature of Antarctic icebergs and the surrounding surface water. Annals of Glaciology, 1, 19–22. https://doi.org/10.3189/S026030550001689X
Orheim, O. (1978). Hvorfor er de Antarktiske isfjell så store? Naturen, 102(6), 277–280.
Orheim, O. (1977). Global glacier mass balance variations during the past 300 years (M. J. Dunbar, Ed.). Arctic Institute of North America.
Robin, G. de Q., & Hisdal, V. (1958). Seismic shooting and related investigations. In Glaciology III (Vol. 5, pp. 1–134). Norsk Polarinstitutt.
Swithinbank, C., & Hisdal, V. (1958). Ice movement inland. In Glaciology I (Vols. 3, F, pp. 150–158). Norsk Polarinstitutt.
Swithinbank, C., & Hisdal, V. (1958). The movement of the ice shelf at Maudheim. In Glaciology I (Vols. 3, C, pp. 82–95). Norsk Polarinstitutt.
Swithinbank, C., & Hisdal, V. (1958). The regime of the ice sheet of western Dronning Maud Land as shown by stake measurements. In Glaciology I (Vols. 3, E, pp. 126–143). Norsk Polarinstitutt.
Swithinbank, C., & Hisdal, V. (1957). The morphology of the ice shelves of western Dronning Maud Land. In Glaciology I (Vols. 3, A, p. [1]-37). Norsk Polarinstitutt.
Swithinbank, C., & Hisdal, V. (1957). The regime of the ice shelves at Maudheim as shown by stake measurements. In Glaciology I (Vols. 3, B, pp. 46–74). Norsk Polarinstitutt.

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