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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Topic

meteorologi

Results 166 resources

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Abstracts

Harsson, B. G. (1971). The 2nd tropopause : a statistical and physical study (Vol. 155). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173710

View on brage.npolar.no
Robin, G. de Q., Hisdal, V., & Hisdal, V. (1971). Upper wind. In Meteorology I (Vols. 1, Part 1D. Aerology, pp. 145–173). Norsk Polarinstitutt.
Kvinge, T. (1970). International Weddell Sea oceanographic expedition : position and weather journal USCGC Glacier (Vol. 22). University of Bergen.
Kvinge, T. (1969). IWSOE - 69 : position and weather journal USCGC “Glacier” (Vol. 18). University of Bergen.
Gjessing, Y. (1967). Tredje etappe av Dronning Maud Land Traversen. In Norsk Polarinstitutt. Årbok 1967 (pp. 233–237). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172795

View on brage.npolar.no
Quartermain, L. B. (1967). The first settlers. In South to the Pole : the early history of the Ross Sea sector, Antarctica (pp. 61–71). Oxford University Press.
Vinje, T. E. (1967). Some features of the turbulence over a snow field. Polar Meteorology : WMO/SCAR/ICPM Symposium on Polar Meteorology, 87, 80–88.
Vinje, T. E. (1967). Some results of micrometeorological measurements in Antarctica. Archiv Für Meteorologie, Geophysik Und Bioklimatologie, Serie A, 16(1), 31–43. https://doi.org/10.1007/BF02246683

View on doi.org
Dybvadskog, O. (1966). Fra Sydpolen til “Utilgjengelighetens pol” (From The South Pole to The Pole of Inaccessibility). In Norsk Polarinstitutt. Årbok 1964 (pp. 165–177). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172801

View on brage.npolar.no
Orheim, O. (1966). Lave temperaturer i Antarktis. Polarboken, 1965/66, 92–94.
Climate data for Norway Station and SANAE in the Antarctic for the years 1960 to 1965. (1965). Weather Bureau. Department of Transport.

This table contains data for Norway Station from January 1960 to January 1962 inclusive, and for SANAE from April (or in some cases June) 1962 to December 1965. A Norwegian type of screen, equipped with a fan, is used for housing the instruments. Air temperatures are measured by means of mercury, thallium and alcohol thermometers; and humidity readings are derived from the records of a Foxboro temperature and dew-point recorder, and sometimes also a hair hygrograph. Wind direction and speed at a height of 10 meters are obtained from a Munro type cup anemometer recording indoors. For the measurement of sunshine, a Fuess-type recorder with two glass spheres and a built-in heater is used. Barometric pressure is obtained from an ordinary Kew-type mercury barometer. (Auth.)
Orheim, O. (1965). Annen etappe av Dronning Maud Land Traversen. In Norsk Polarinstitutt. Årbok 1965 (pp. 184–186). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/172751

View on brage.npolar.no
Vinje, T. E. (1964). On the radiation balance and micrometeorological conditions at Norway station, Antarctica (Vol. 131). Norsk Polarinstitutt. https://urn.nb.no/URN:NBN:no-nb_digibok_2007032701054

View on urn.nb.no
Giæver, J., Schytt, V., & Hisdal, V. (1963). General report of the expedition. In Geology, biology & general report of the expedition (Vols. 6, Part 3, p. [1]-41). Norsk Polarinstitutt.
Hagen, K., & Hisdal, V. (1963). The surface inversion. In Meteorology I (Vols. 1, Part 1C. Aerology, pp. 128–139). Norsk Polarinstitutt.
Schumacher, N. J., & Hisdal, V. (1962). The tropopause. In Meteorology I (Vols. 1, Part 1B. Aerology, pp. 100–123). Norsk Polarinstitutt.
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.

View on hdl.handle.net
Luncke, B. (1959). Norsk Polarinstitutts målevirksomhet. Norsk tidsskrift for jordskifte og landmåling, 51(4–5), 439–442.
Schumacher, N. J., & Hisdal, V. (1958). Temperature, height and humidity. In Meteorology I (Vols. 1, Part 1A. Aerology, p. [1]-94). Norsk Polarinstitutt.
Robin, G. de Q. (1957). Upper winds over an Antarctic Station. Quarterly Journal of the Royal Meteorological Society, 83(358), 533–537.

Preliminary results from the Norwegian-British-Swedish Antarctic expedition 1949-52. A preliminary note on the upper-air temperatures over Maudheim, the base of the Norwegian-British-Swedish Antarctic Expedition 1949-1952, has already been published by Nils Jorgen Schumacher (1955). This note is intended to throw further light on some points raised in Schumacher's paper and to outline the general pattern of upper winds over Maudheim. Owing to the use of a radio theodolite, the data gave a representative picture of the wind structure over an Antarctic station without the excessive bias of previous observations which were limited to periods of clear weather. The detailed report and discussion of aerological observations made at Maudheim will be published shortly by the Norwegian Polar Institute.

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