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  • 41. ces-glacier-scaling-memo2009-01

    magnitude of other errors in a basin-wide analysis as described here. Model description The model proposed here is intended to capture the most important characteristics of the cu- mulative response of many glaciers of different sizes within a single watershed to mass balance changes without the need for detailed dynamic modelling of each glacier. The focus is on glacier retreat, temporary /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 42. Reports and publications

    usage summary - First 6 months: February 1 - July 31, 2003 (PDF) Ragnar Stefánsson, Barði Þorkelsson 13 0,8 2002 Seismicity in Iceland 1991-2000 monitored by the SIL seismic system (PDF) Steinunn S. Jakobsdóttir, Gunnar B. Guðmundsson, Ragnar Stefánsson 8 3,4 2002 Application - PREPARED, B- og C-hluti umsóknar (PDF) Ragnar Stefánsson et al. 97 0.5 2002 PREPARED - Description /earthquakes-and-volcanism/reports-and-publications/
  • 43. Grímsvötn 2010

    outburst flood in 2010 3.11.2010 Jökulhlaup from Grímsvötn subsides - 5 November 2010 The jökulhlaup (glacial outburst flood) from Grímsvötn that began near the end of October is now coming to an end. See thorough description in news on front page. Assessment - 5 /hydrology/articles/nr/2040
  • 44. UST_table_SO2_27112014-en

    Air quality description Recommended actions µg/m3 ppm All children. Sensitive Groups * Healthy individuals Good 0-350 0-0,1 Poses little or no health risk. Can experience mild respiratory symptoms. No health effects expected. Moderate 350-600 0,1-0,2 May cause respiratory symptoms in individuals with underlying diseases. Caution advised. Follow SO2 measurements closely /media/jar/UST_table_SO2_27112014-en.pdf
  • 45. Grímsvötn 2010

    outburst flood in 2010 3.11.2010 Jökulhlaup from Grímsvötn subsides - 5 November 2010 The jökulhlaup (glacial outburst flood) from Grímsvötn that began near the end of October is now coming to an end. See thorough description in news on front page. Assessment - 5 /earthquakes-and-volcanism/articles/nr/2040
  • 46. CES_D2.4_task2_CMIP3_winds

    parameterization and surface description (e.g., land-sea distribution, sea ice cover, roughness and orography) in the models. Thus, the use of the geostrophic wind speed that is proportional to the surface pressure gradient allows a more straightforward comparison among the models and to observational data. For the analyses reported here, all model results were interpolated onto a common 2.5° × 2.5 /media/ces/CES_D2.4_task2_CMIP3_winds.pdf
  • 47. 2011_005

    and a short description for each network. Table 1. The CGPS sub-networks. Network name Short background CHIL University of Iceland, University of Arizona, and IMO Hekla Penn State University and IMO ISGPS IMO and foreign associates NICE ETH, Zürich and IMO Savoie University of Savoie and IMO Semi-CGPS University of Iceland, University of Savoie, and IMO 1.6 Other networks Table 2 /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
  • 48. Paper-Olafur-Rognvaldsson_91

    is done by using the mesoscale MM5 model (Grell et al., 1995). This paper begins with a description of the model approach, followed by comparison of the model results to data and concluding remarks. MODELLING WITH THE MM5 MODEL The idea of using limited area models (LAMs) for regional climate simula- tions was introduced by Dickinson et al. (1989) and refined by Giorgi (1990). One of the benefits /media/ces/Paper-Olafur-Rognvaldsson_91.pdf
  • 49. Past temperature conditions in Iceland

    being 1995. Since then it has been warm, the warmth culminating in 2002 to 2003. Generally the description above refers to the whole country, but there are slightly diverging details, depending on the source of the cold air. Back to top Comparison of temperature in Stykkishólmur, Akureyri and Reykjavík A comparison of annual temperatures at three stations, Stykkishólmur in the west, Akureyri /climatology/articles/nr/1213
  • 50. Past temperature conditions in Iceland

    being 1995. Since then it has been warm, the warmth culminating in 2002 to 2003. Generally the description above refers to the whole country, but there are slightly diverging details, depending on the source of the cold air. Back to top Comparison of temperature in Stykkishólmur, Akureyri and Reykjavík A comparison of annual temperatures at three stations, Stykkishólmur in the west, Akureyri /climatology/articles/nr/1213/

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