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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"Orheim, Olav"

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Abstracts

Orheim, O., & Lucchitta, B. (1990). Investigating Climate Change by Digital Analysis of Blue Ice Extent on Satellite Images of Antarctica. Annals of Glaciology, 14, 211–215. https://doi.org/10.3189/S0260305500008600
Orheim, O., & Drewry, D. (1986). Flow and thickness of Riiser-Larsenisen, Antarctica. In Glaciological research on Riiser-Larsenisen and nearby ice-shelves in Antarctica (Vol. 187, pp. 5–22). Norsk Polarinstitutt. http://hdl.handle.net/11250/173516

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Kristensen, M., & Orheim, O. (1985). Iceberg research and other glaciological studies from K/V “Andenes.” In Report of the Norwegian Antarctic research expedition (NARE) 1984/85 (Vol. 22, pp. 127–138). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173240

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Orheim, O., & Elverhøi, A. (1981). Model for submarine glacial deposition. Annals of Glaciology, 2, 123–128. https://doi.org/10.3189/172756481794352135
Orheim, O. (2000). The Committee for Environmental Protection: Its Establishment, Operation and Role within the Antarctic Treaty System. In D. Vidas (Ed.), Implementing the Environmental Protection Regime for the Antarctic (Vol. 28, pp. 107–124). Kluwer Academic Publishers.
Orheim, O. (1993). The place of regulation in relation to science. In A. Elzinga (Ed.), Changing trends in Antarctic research (Vol. 3, pp. 55–60). Kluwer Academic Publishers.
Norsk, P. (1990). Report of the Norwegian Antarctic Research Expedition 1989/90 (O. Orheim, Ed.; Vol. 113). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Orheim, O., & Lucchitta, B. K. (1987). Snow and Ice Studies By Thematic Mapper and Multispectral Scanner Landsat Images. Annals of Glaciology, 9, 109–118. https://doi.org/10.3189/S0260305500000483
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
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

This paper presents mass-balance results from Deception Island for 1968–69 to 1973–74, from King George Island for the balance years 1969–70 and 1970–71, and from Livingston Island from 1971–72 to 1973–74. The accumulation areas of all localities are in the soaked fades, with a firn/ice transition at King George Island at 12 to 20 m depth. Of the glaciers studied, only “Gl” on Deception Island terminates wholly on land and has a relatively large ablation area. The mass-balance curves are similar for King George Island and Livingston Island, with equilibrium lines at around 150 m elevation. “Gl“ on Deception Island has more negative summer balances, and the equilibrium line ranged from 275 to 370 m during the six balance years. Here, there were no years of positive net mass balance, and large negative net values during the 1970–71 to 1972–73 balance years. This resulted from a lowered albedo caused by ash from the August 1970 eruption. Ash layers from the Deception Island eruptions are also observed on Livingston Island and King George Island, where they form stratigraphic markers in the accumulation areas of the glaciers. Annual balance variations from 1957–58 to 1970–71, based on stratigraphic studies at Deception Island and King George Island, show good correlations, indicating that the variations reflect changes in regional climate.
Orheim, O. (1977). Global glacier mass balance variations during the past 300 years (M. J. Dunbar, Ed.). Arctic Institute of North America.
Kläy, J.-R., & Orheim, O. (1969). Glaciology and glacial geology on Deception Island. Antarctic Journal of the United States, 4(4), 125–126.
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

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Orheim, O. (ed. ), & Brekke, A. (ed. ). (1989). Hva skjer med klimaet i polarområdene? : sammendrag av foredrag på symposium 25-26 april 1989 (Vol. 53). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173488

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Orheim, O., Wadhams, P., & Kristensen, M. (1982). Iceberg response to sea state (abstract only). Annals of Glaciology, 3, 357. https://doi.org/10.3189/S0260305500003360
Kristensen, M., Orheim, O., & Wadhams, P. (1981). Field experiments on Antarctic tabular icebergs. Polar Record, 20(128), 445–448. https://doi.org/10.1017/S0032247400003661
Orheim, O., Wadhams, P., & Kristensen, M. (1982). Iceberg response to sea state. Iceberg Research, 1, 10–15.
Wadhams, P., Kristensen, M., & Orheim, O. (1983). The response of Antarctic icebergs to ocean waves. Journal of Geophysical Research: Oceans, 88(C10), 6053–6065. https://doi.org/10.1029/JC088iC10p06053

The heave, tilt, and strain responses of three Antarctic tabular icebergs to ocean waves were measured during a 1980–1981 cruise of HMS Endurance to the South Atlantic. The three icebergs, located near the South Sandwich and South Orkney islands, were instrumented with accelerometers, tiltmeters, and wire strainmeters, while a Waverider buoy was used to record the ocean wave field. The thickness of the icebergs was surveyed by a helicopter-borne radio echo sounder. The heave response occurred mainly at the swell period but with outbreaks of bobbing which lasted for a few cycles at a resonant period (about 40 s), which agreed well with the predictions of a numerical finite element model. The roll response occurred mainly at a long resonant period (40–50 s), which again agreed well with the model, but there was also a significant response at ocean wave periods (5–20 s), which exceeded predictions. The strain response had a component at very long periods, which is unexplained by theory, while the surface strain at ocean wave periods agreed with the simple analytical model of Goodman et al. (1980). Using this model it is possible to predict a wave height and period that will cause breakup of the icebergs, and we conclude that swell-induced breakup is likely to occur during major storms in the open southern ocean.

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Kovacs, K. M. (2011). Seler brukt som “forskningsassistenter” for å utforske polhavene. In O. Orheim & K. Ulstein (Eds.), Polaråret 2007-2008 : det norske bidraget (pp. 101–103). Norges forskningsråd. https://doi.org/oai:nb.bibsys.no:991122954014702202 URN:NBN:no-nb_digibok_2014120907592

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Iversen, S. A. (2011). Krill og økosystemtokt med G.O.Sars i Sørishavet. In O. Orheim & K. Ulstein (Eds.), Polaråret 2007-2008 : det norske bidraget (pp. 97–99). Norges forskningsråd. https://doi.org/oai:nb.bibsys.no:991122954014702202 URN:NBN:no-nb_digibok_2014120907592

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