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

Page 105 of 145

Abstracts

Lunde, E. (1962). Norges “tapte kontinenter” I. Nå, 11(8), 8–11. https://urn.nb.no/URN:NBN:no-nb_digitidsskrift_2019011781974_001

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Price, A. G. (ed. ). (1962). The Winning of Australian Antarctica: Mawson’s BANZARE voyages, 1929-31, based on the Mawson Papers. Angus and Robertson.
Schumacher, N. J., & Hisdal, V. (1962). The tropopause. In Meteorology I (Vols. 1, Part 1B. Aerology, pp. 100–123). Norsk Polarinstitutt.
Swithinbank, C. (1962). Maudheim Revisited: The Morphology and Regime of the lce Shelf, 1950-1960. In N. Heintz (Ed.), Norsk Polarinstitutt. Årbok 1960 (pp. 28–31). Norsk Polarinstitutt. http://hdl.handle.net/11250/172773

Maudheim, the base of the Norwegian-British-Swedish Antarctic Expedition, 1949-52, (71° 02' S, 10° 56' W) was revisited in January 1960 by the Norwegian Antarctic Expedition, 1956-60 under the leadership of SIGURD HELLF.. HELLE has very kindly made his observations available to me and has read the manuscript of this note. The work of his party gives a reliable measure of the accumulation of snow at Maudheim from 1952 to 1960 and allows a hetter estimate of the bottom melting on the ice shelf than was possible from the 1950-52 measurements. Air photographs taken in December 1958 by B. LuNCKE show the extent of changes in the ice front since 1951.

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Vinje, T. E. (1962). The cooling power in Antarctica. In N. Heintz (Ed.), Norsk Polarinstitutt. Årbok 1961 (pp. 7–22). Norsk Polarinstitutt. http://hdl.handle.net/11250/172823

We have measured the cooling power at Norway Station (70°.5 S, 2°.5 W)with kata-thermometers for air-temperature (Ta) between + 1 and --41° C, and for wind speeds (v) at 10 m leve! up to 27 m sec-1• The linear proportionality of the cooling power (H) to (36.5-Ta), for a constant wind speed, is shown to hold in this temperature-interval for a wind speed less than about 12 m sec-1• We used four kata-thermometers, and it turned out that they gave systematic different values of the cooling power for equal meteorological conditions. Comparing the individual values with their mean we find a maximum deviation of about ± 20 % . W e have supposed that this is due to errors in the calibration, subjective errors plus dissimilarities in the shape of the bulbs. The latter will cause differences in the turbulence around the bulbs, and consequently in the effective cooling of the wind. The possible difference in the cooling power of the air due to differences in the shape will probably not emerge during calibrations in a still air chamber. In spite of the dissimilar climatic conditions in Antarctica and Europe we found that a formula based upon two of our Katas, with which we have taken by far the most measurements, corresponds fairly well to the mean of the Kata-formulae found in Europe. The maximum deviation of the values given by European formulae from those derived by the Norway Station formula is about ± 20 %. We have here omitted the formula of HILL (1919), as it reveals a fairly large deviation from the other formulae.

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Wilson, O. (1962). Basal metabolic rate of “tropical” man in a polar climate. In S. W. Tromp (Ed.), Biometeorology: Proceedings of the Second International Bioclimatological Congress Held at the Royal Society of Medicine, London, 4–10 Sept. 1960, Organized by “The International Society of Biometeorology” (pp. 411–426). Pergamon. https://doi.org/https://doi.org/10.1016/B978-0-08-009683-4.50055-3

Naked man in his mode of heat regulation can be regarded as a tropical or subtropical creature with a narrow zone of adaptability, and the difference in the BMR determined in the tropics and in a temperate zone for the same individuals does not seem to exceed 10 per cent. In the climatic extremes he raises his calorific output in situations of stress but does not adapt by further changing his BMR. Some native people, however, appear to have the ability to endure a moderate cold stress without increasing their heat production above normal basal values. The metabolic determinations made by the author on the Norwegian—British–Swedish Expedition during 2 years of continuous exposure to the Antarctic climate show that there is no difference in the mean level of the BMR of white man whether he lives in a temperate or a polar climate. Other studies in cold regions support this view. Evidence of acclimatization of man to cold will not be found in the basal metabolic rate. However, the author's investigations show that the polar climate in its extreme form, as it is encountered by man in the Antarctic, can impose certain seasonal variations in the BMR. This periodicity in BMR is probably not a direct effect of climate on metabolism, but is related to it by reason of the typical activity pattern which ensues in the Antarctic climate. In agreement are the seasonal changes in BMR in the Arctic reported by Russian workers. The preliminary results of Lewis and Masterton in North Greenland, on the other hand, do not indicate a consistent seasonal variation. In changing from a temperate to a tropical climate, the BMR may vary within a narrow range of about 10 per cent, decreasing in the hot environment, but not all persons will show such a change. The seasonal variation found by the author in a polar climate is almost of the same order as the change in the tropics. It may be that the alterations in BMR caused by a change to a tropical climate are due to similar influences, which, however, do not exhibit the same seasonal incidence, because of the uniformity of the climate the year around. This implies that the basal metabolism of white man is essentially the same in all climates, but varies within a narrow range, not as a direct result of climate itself or its mean temperature, but depending upon changes in the type of activity, food, exposure, muscle tone and other factors, which are imposed by a difference in climate and regimen.

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Zenkovich, B. A. (1962). Sjøpattedyr observert av det sovjetiske vitenskapsakademis ekspedisjon rundt jorden i 1957/58. Norsk hvalfangst-tidende, 51(5), 198–210.
Ahlmannryggen: Fimbulheimen. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/d0c038c4-ae91-5fc3-a35c-826e38426ee5

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H.U.Sverdrupfjella: Fimbulheimen. (1961). [Map]. Norsk Polarinstitutt. https://data.npolar.no/map/archive/5a9a4b4f-e1a3-5ad4-9237-69bacb8cf93d

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Jutulgryta: Fimbulheimen. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/ef8e9d72-2e8c-5c7a-9760-5e823c3480fa

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Jutulgryta: Fimbulheimen. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/ef8e9d72-2e8c-5c7a-9760-5e823c3480fa

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Jutulstraumen: Maudheimvidda. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/490ac06a-d182-5a0c-9727-0d5d00276f60

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Kirwanveggen: Maudheimvidda. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/ae8e2f39-6a72-5eb9-b095-be1b2f645c3c

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Neumayerskarvet: Maudheimvidda. (1961). [Map]. Norsk Polarinstitutt; Norwegian Polar Data Centre. https://data.npolar.no/map/archive/013f646d-dca7-515b-baa1-bfcc61ad7e45

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Broch, H. (1961). Benthonic problems in Antarctic and Arctic waters. Aschehoug. https://doi.org/oai:nb.bibsys.no:999524623974702202 URN:NBN:no-nb_digibok_2014102208103

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Eriksen, E. (1961). Tønsbergs sjøfart gjennom 100 år. Vestfoldminne, 1961, 5–12. https://doi.org/oai:urn.nb.no:no-nb_digitidsskrift_2019071081170_001 URN:NBN:no-nb_digitidsskrift_2019071081170_001

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Fjeld-Andersen, A. (1961). Oversiktskatalog 1 : over bøker, periodiske skrifter og særtrykk ved Hvalfangstmuseets bibliotek (Vol. 25). Hvalfangstmuseum. https://doi.org/oai:nb.bibsys.no:999617202634702202 URN:NBN:no-nb_digibok_2017021608129

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Gran, T. (1961). Kampen om Sydpolen. Mortensen. https://doi.org/oai:nb.bibsys.no:999206751234702202 URN:NBN:no-nb_digibok_2007031401031

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Henriksen, B. (1961). Polarfareren Hjalmar Johansen og Skien. B. Henriksen. https://doi.org/oai:nb.bibsys.no:999217899804702202 URN:NBN:no-nb_digibok_2014021006096

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Lunde, T. (1961). On the snow accumulation in Dronning Maud Land (Vol. 123). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999104154984702202 URN:NBN:no-nb_digibok_2007050201009

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