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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"Hagen, Jon-Ove"

Results 12 resources

Abstracts

Hagen, J. O., & Melvold, K. (1997). Mass balance and dynamics on Jutulstraumen ice stream. In Report of the Norwegian Antarctic Research Expedition 1992/93 (Vol. 125, pp. 85–92). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173096

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Thomsen, H. H., & Hagen, J. O. (1997). A stable isotope pilot study from blue ice areas at Jutulsessen, Dronning Maud Land, Antarctica. In Report of the Norwegian Antarctic Research Expedition 1992/93 (Vol. 125, pp. 104–110). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173096

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Orheim, O., Hagen, J. O., Østerhus, S., & Sætrang, A. (1990). Studies on, and underneath, the Ice Shelf Fimbulisen. In Report of the Norwegian Antarctic Research Expedition 1989/90 (Vol. 113, pp. 59–73). Norsk Polarinstitutt. https://doi.org/oai:nb.bibsys.no:999101870964702202 URN:NBN:no-nb_digibok_2007102600009

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Orheim, O., Hagen, J. O., Østerhus, S., & Sætrang, A. (1990). Glaciologic and oceanographic studies on Fimbulisen during NARE 1989/90. Filchner-Ronne Ice Shelf Programme. Report, 4, 120–131.
Melvold, K., Hagen, J. O., Laumann, T., & Tonning, T. (1996). Mass balance and dynamics on Jutulstraumen ice stream during NARE 1993/94. In Report of the Norwegian Antarctic Research Expedition 1993/94 (Vol. 140, pp. 19–23). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173094

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Melvold, K., Hagen, J. O., Pinglot, J. F., & Gunuestrup, N. (1998). Large spatial variation in accumulation rate in Jutulstraumen ice stream, Dronning Maud Land, Antarctica. Annals of Glaciology, 27, 231–238. https://doi.org/10.3189/1998AoG27-1-231-238

A mass-balance programme was initiated on Jutulstraumen ice stream, western Dronning Maud Land,Antarctica, during the austral summer 1992-93. As a part of the mass-balance programme, accumulation rate was measured along the centre line of Jutulstraumen from the shelf edge up to the plateau at about 2500 m a.s.l. Accumulation distribution obtained from seven shallow firn cores and 48 slake readings is presented. The overall net accumulation trend displays a decreasing accumulation with increasing elevation and distance to coast, but on both the mesoscale and microscale there are significant variations. This is due to complex patterns of precipitation controlled by orography and redistribution by katabatic winds. The local accumulation distribution (few km scale) was found to be dependent on downslope surface gradient (aspect north, northwest), and variations up to 100% were found over distances of less than 3 km. The large variation in accumulation is important when selecting new core sites and for interpretation of temporal and spatial variations in accumulation derived from firn cores.

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Rolstad, C., Whillans, I. M., Hagen, J. O., & Isaksson, E. (2000). Large-scale force budget of an outlet glacier: Jutulstraumen, Dronning Maud Land, East Antarctica. Annals of Glaciology, 30, 35–41. https://doi.org/10.3189/172756400781820642

A large-scale force budget was applied using a combination of remote-sensing and field data from Jutulstraumen, Dronning Maud Land, Antarctica. In the grounded area, more than 95 % of ice flow is balanced by basal friction. In a partly floating section near the grounding-line area, on average lateral drag provides 38% of resistance to flow. Measurement uncertainties were propagated through the calculation of forces. The accuracies of strain rates derived from satellite data (Landsat thematic mapper) were found adequate to calculate meaningful force-balance terms. For the floating section, where lateral forces contribute to controlling flow, the main contribution to errors in the force budget is uncertainty in the rate factor for the flow law of ice. For grounded sections, the uncertainty in ice thickness, as measured by ground-penetrating radar, contributes more or less equally to errors in the force budget as does that in the rate factor.
Müller, K., Albert, M., Hamran, S. E., & Hagen, J. O. M. (2008). Radar Scattering Zones across Dronning Maud Land, East Antarctica. International Glaciological Society.
Melvold, K., Hagen, J. O., Laumann, T., & Rolstad, C. (1997). Mass balance and dynamics on Jutulstraumen ice stream, NARE 1996/97. In J.-G. (ed. ) Winther (Ed.), Report of the Norwegian Antarctic Research Expedition 1996/97 (Vol. 148, pp. 118–124). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173024

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Müller, K., Sinisalo, A., Anschütz, H., Hamran, S.-E., Hagen, J.-O., McConnell, J. R., & Pasteris, D. R. (2010). An 860 km surface mass-balance profile on the East Antarctic plateau derived by GPR. Annals of Glaciology, 51(55), 1–8. https://doi.org/10.3189/172756410791392718

Snow accumulation and its variability on the East Antarctic plateau are poorly understood due to sparse and regionally confined measurements. We present a 5.3 GHz (C-band) ground-penetrating radar (GPR) profile with a total length of 860 km recovered during the joint Norwegian–US International Polar Year traverse 2007/08. Mean surface mass balance (SMB) over the last 200 years was derived from the GPR data by identifying the volcanic deposition of the Tambora eruption in 1815. It varies between 9.1 and 37.7 kg m−2 a−1 over the profile, with a mean of 23.7 kg m−2 a−1 and a standard deviation of 4.7 kg m−2 a−1. The 200 year SMB estimated is significantly lower than most of the SMB estimates over shorter time periods in this region. This can be partly explained by a SMB minimum in the vicinity of the ice divide. However, it is more likely that a recent increase in SMB observed by several studies is largely responsible for the observed discrepancy.
Rolstad, C., Hagen, J. O., Østen, K., Tonning, T., & Semb, S. I. (1999). A study of the ice dynamics of Jutulstraumen drainage area, by means of remote sensing. In T. (ed. ) Tveraa & J.-G. (ed. ) Winther (Eds.), Report of the Norwegian Antarctic Research Expedition 1997/98 (Vol. 156, pp. 19–25). Norsk Polarinstitutt. https://brage.npolar.no/npolar-xmlui/handle/11250/173073

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Sinisalo, A., Anschütz, H., Aasen, A. T., Langley, K., von Deschwanden, A., Kohler, J., Matsuoka, K., Hamran, S.-E., Øyan, M.-J., Schlosser, E., Hagen, J. O., Nøst, O. A., & Isaksson, E. (2013). Surface mass balance on Fimbul ice shelf, East Antarctica: Comparison of field measurements and large-scale studies. Journal of Geophysical Research: Atmospheres, 118(20), 11, 611–625, 635. https://doi.org/https://doi.org/10.1002/jgrd.50875

Many challenges remain for estimating the Antarctic ice sheet surface mass balance (SMB), which represents a major uncertainty in predictions of future sea-level rise. Validating continental scale studies is hampered by the sparse distribution of in situ data. Here we present a 26 year mean SMB of the Fimbul ice shelf in East Antarctica between 1983–2009, and recent interannual variability since 2010. We compare these data to the results of large-scale SMB studies for similar time periods, obtained from regional atmospheric modeling and remote sensing. Our in situ data include ground penetrating radar, firn cores, and mass balance stakes and provide information on both temporal and spatial scales. The 26 year mean SMB on the Fimbul ice shelf varies between 170 and 620 kg m−2 a−1 giving a regional average value of 310 ± 70 kg m−2 a−1. Our measurements indicate higher long-term accumulation over large parts of the ice shelf compared to the large-scale studies. We also show that the variability of the mean annual SMB, which can be up to 90%, can be a dominant factor in short-term estimates. The results emphasize the importance of using a combination of ground-based validation data, regional climate models, and remote sensing over a relevant time period in order to achieve a reliable SMB for Antarctica.

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