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  • Active layer depth; Area/locality; Comment; Dalsnibba/Dal; Degree days, freezing; Degree days, thawing; Depth, reference; Description; Dovrefjell/DBl; Elevation of event; Endalen/EN-B-1; Event label; Finland; Gagnheidi; Gruvefjellet/GF-B-1; Guolasjavri1/Gu-B-l; Hagongur; Iceland; International Polar Year (2007-2008); IPY; Iskoras1/Is-B-l; Iskoras2/Is-B-2; Janssonhaugen/1099; Jettabhl/Jet-BHl; JuvvashøeBH31/PACE31; Juvvassbh2/Juv-BH2; Juvvassbh3/Juv-BH3; Juvvassbhl/Juv-BHl; KappLinné1/KL-B-l; KappLinné2/KL-B-2; KappLinné3/KL-B-3; Kistefjellet/Ki-B-1; Kursflaket/KF-1; Kursflaket/KF-2; Latitude of event; Lavkavagge1/La-B-l; Longitude of event; MULT; Multiple investigations; Name; Norway; Ny-Ålesund, Spitsbergen; Ny-Ålesund/NA-B-1; OldAuroralStation2/AS-B-2; Operation mode; Saudafell; Snowdrift1/SN-B-l; Snowdrift2/SN-B-2; Snow thickness; Storflaket/SF-1; Storflaket/SF-2; Storflaket/SF-3; Svalbard; Svea2/Sv-B-2; Svea5/Sv-B-5; Sweden; Tarfalaryggen/Ta-1; Tarfalaryggen/Ta-2; Tavvavuoma/T10; Tavvavuoma/T2; Temperature, air, annual mean; Temperature, ground, annual mean; Temperature recorder; TEMP-R; Time coverage; Torneträsk, Sweden; Tronbhl/Tro-BHl; Vaisjeaggi1/Va-l; ZAC; Zackenberg; Zackenberg, Northeast Greenland  (1)
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  • Active layer depth; Area/locality; Comment; Dalsnibba/Dal; Degree days, freezing; Degree days, thawing; Depth, reference; Description; Dovrefjell/DBl; Elevation of event; Endalen/EN-B-1; Event label; Finland; Gagnheidi; Gruvefjellet/GF-B-1; Guolasjavri1/Gu-B-l; Hagongur; Iceland; International Polar Year (2007-2008); IPY; Iskoras1/Is-B-l; Iskoras2/Is-B-2; Janssonhaugen/1099; Jettabhl/Jet-BHl; JuvvashøeBH31/PACE31; Juvvassbh2/Juv-BH2; Juvvassbh3/Juv-BH3; Juvvassbhl/Juv-BHl; KappLinné1/KL-B-l; KappLinné2/KL-B-2; KappLinné3/KL-B-3; Kistefjellet/Ki-B-1; Kursflaket/KF-1; Kursflaket/KF-2; Latitude of event; Lavkavagge1/La-B-l; Longitude of event; MULT; Multiple investigations; Name; Norway; Ny-Ålesund, Spitsbergen; Ny-Ålesund/NA-B-1; OldAuroralStation2/AS-B-2; Operation mode; Saudafell; Snowdrift1/SN-B-l; Snowdrift2/SN-B-2; Snow thickness; Storflaket/SF-1; Storflaket/SF-2; Storflaket/SF-3; Svalbard; Svea2/Sv-B-2; Svea5/Sv-B-5; Sweden; Tarfalaryggen/Ta-1; Tarfalaryggen/Ta-2; Tavvavuoma/T10; Tavvavuoma/T2; Temperature, air, annual mean; Temperature, ground, annual mean; Temperature recorder; TEMP-R; Time coverage; Torneträsk, Sweden; Tronbhl/Tro-BHl; Vaisjeaggi1/Va-l; ZAC; Zackenberg; Zackenberg, Northeast Greenland  (1)
  • multi-compartment elimination  (1)
  • *Ice  (1)
  • *Planets  (1)
  • *Stars, Celestial  (1)
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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Christiansen, Hanne Hvidtfeldt; Etzelmüller, Bernd; Isaksen, Ketil; Juliussen, H; Farbrot, Herman; Humlum, Ole; Johansson, M; Ingeman-Nielsen, Thomas; Kristensen, L; Hjort, J; Holmlund, Per; Sannel, A Britta K; Sigsgaard, C; Åkerman, H J; Foged, N; Blikra, Lars Harald; Pernosky, M A; Ødegård, Rune Strand (2010): The Thermal State of Permafrost in the Nordic Area during the International Polar Year 2007-2009. Permafrost and Periglacial Processes, 21(2), 156-181, https://doi.org/10.1002/ppp.687
    Publication Date: 2023-12-13
    Description: This paper provides a snapshot of the permafrost thermal state in the Nordic area obtained during the International Polar Year (IPY) 2007-2009. Several intensive research campaigns were undertaken within a variety of projects in the Nordic countries to obtain this snapshot. We demonstrate for Scandinavia that both lowland permafrost in palsas and peat plateaus, and large areas of permafrost in the mountains are at temperatures close to 0°C, which makes them sensitive to climatic changes. In Svalbard and northeast Greenland, and also in the highest parts of the mountains in the rest of the Nordic area, the permafrost is somewhat colder, but still only a few degrees below the freezing point. The observations presented from the network of boreholes, more than half of which were established during the IPY, provide an important baseline to assess how future predicted climatic changes may affect the permafrost thermal state in the Nordic area. Time series of active-layer thickness and permafrost temperature conditions in the Nordic area, which are generally only 10 years in length, show generally increasing active-layer depths and rising permafrost temperatures.
    Keywords: Active layer depth; Area/locality; Comment; Dalsnibba/Dal; Degree days, freezing; Degree days, thawing; Depth, reference; Description; Dovrefjell/DBl; Elevation of event; Endalen/EN-B-1; Event label; Finland; Gagnheidi; Gruvefjellet/GF-B-1; Guolasjavri1/Gu-B-l; Hagongur; Iceland; International Polar Year (2007-2008); IPY; Iskoras1/Is-B-l; Iskoras2/Is-B-2; Janssonhaugen/1099; Jettabhl/Jet-BHl; JuvvashøeBH31/PACE31; Juvvassbh2/Juv-BH2; Juvvassbh3/Juv-BH3; Juvvassbhl/Juv-BHl; KappLinné1/KL-B-l; KappLinné2/KL-B-2; KappLinné3/KL-B-3; Kistefjellet/Ki-B-1; Kursflaket/KF-1; Kursflaket/KF-2; Latitude of event; Lavkavagge1/La-B-l; Longitude of event; MULT; Multiple investigations; Name; Norway; Ny-Ålesund, Spitsbergen; Ny-Ålesund/NA-B-1; OldAuroralStation2/AS-B-2; Operation mode; Saudafell; Snowdrift1/SN-B-l; Snowdrift2/SN-B-2; Snow thickness; Storflaket/SF-1; Storflaket/SF-2; Storflaket/SF-3; Svalbard; Svea2/Sv-B-2; Svea5/Sv-B-5; Sweden; Tarfalaryggen/Ta-1; Tarfalaryggen/Ta-2; Tavvavuoma/T10; Tavvavuoma/T2; Temperature, air, annual mean; Temperature, ground, annual mean; Temperature recorder; TEMP-R; Time coverage; Torneträsk, Sweden; Tronbhl/Tro-BHl; Vaisjeaggi1/Va-l; ZAC; Zackenberg; Zackenberg, Northeast Greenland
    Type: Dataset
    Format: text/tab-separated-values, 479 data points
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    European journal of clinical pharmacology 8 (1975), S. 439-444 
    ISSN: 1432-1041
    Keywords: Methotrexate ; overall elimination half-life ; multi-compartment elimination ; renal function ; serum creatinine ; age effect
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Medicine
    Notes: Summary The disappearance of methotrexate (MTX) from serum was studied using H3-MTX. The overall elimination half-life (MTX T 1/2) was well defined from one to about six hours after i.v. administration; in 25 patients it ranged from 102 min to 750 min and was inversely related to endogenous creatinine clearance, which ranged from 6 to 140 ml/min. The corresponding apparent volume of distribution, V, obtained by extrapolation tended to decrease at lower levels of renal function. The total clearance of MTX calculated in this period varied linearly with creatinine clearance. In patients with normal serum creatinine concentration, the half-life increased with advancing age, which reflects the concurrent age-dependent decrease in creatinine production and renal function. This illustrates the need for knowledge of renal function, not based solely on serum creatinine concentration, in patients treated with methotrexate or other drugs eliminated by the kidneys. In 9 patients the results were not affected by treatment with diuretics (furosemide, hydroflumethiazide). In four patients serum MTX concentration was measured for up to 24–72 hours. An increasing half-life of MTX with time was found, suggesting that the elimination kinetics of the drug would be most adequately described by a multi-compartment model.
    Type of Medium: Electronic Resource
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