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  • 41. 2013_001_Nawri_et_al

    is then proportional to the mean cube of wind speed, E = 1 2 r¯ A3G(1+3=k) ; (3) where r¯ is average air density. Wind power density only depends on atmospheric variables, and is therefore most appropriate for turbine-independent evaluations of wind energy potential, such as for wind atlases. To be able to determine the actual power or energy, which can be extracted from the atmosphere, specific information /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 42. Isskyrsla_06Jan_2010

    8. 66°47,5‘N – 021°59,0‘V 9. 66°55,6‘N – 022°01,7‘V (Austasti punktur sem við mældum) Út frá aðalrönd íssins lágu ís-totur eins og sést á teikningunni. Syðst lá samfrosta ís 10/10 og náði hann SA að stöðum. 1. 66°12,9‘N – 024°47,3‘V 2. 66°14,1‘N – 024°42,2‘V Svo lá gisin ís-tota 4-6/10 frá aðalrönd íssins eins og sést á teikningunni í SA að stöðum. 1. 66°16,0‘N – 24°20,1‘V 2. 66°22,3‘N – 24°12,0‘V /media/hafis/skyrslur_lhg/Isskyrsla_06Jan_2010.pdf
  • 43. Moellenkampetal_etal-2010

    Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Daniell, K. A., I. White, N. Ferrand, I. S. Ribarova, P. Coad, J.-E. Rougier, M. Hare, N. A. Jones, A. Popova, D. Rollin, P. Perez, and S. Burn. 2010. Co-engineering participatory water management processes: theory and insights from Australian and Bulgarian interventions. Ecology and Society 15(4): 11 /media/loftslag/Moellenkampetal_etal-2010.pdf
  • 44. Refsgaard_2-uncertainty

    Geological Survey of Denmark and Greenland Ministry of Climate and Energy NONAM PhD course, Copenhagen, August 22-26, 2011 Uncertainty – terminology, concepts, tools and importance in climate change adaptation Jens Christian Refsgaard Acknowledgements • Torben O. Sonnenborg, GEUS • Hans Jørgen Henriksen, GEUS • Anker Lajer Højberg, GEUS • Peter van der Keur, GEUS • Lieke van Roosmalen, Flinders /media/loftslag/Refsgaard_2-uncertainty.pdf
  • 45. AnneFleig_May2010_CES

    activities. Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “ University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook Hydrological drought in NW-Europe: Data 5 6 5 8 6 0 5 5 . 5 5 6 . 0 5 6 . 5 5 7 . 0 5 7 . 5 -10 -5 0 5 10 15 20 25 3 5 4 0 4 5 5 0 5 5 6 0 6 5 7 0 s o u r c e : N a t i o n a l E n v i r o n m e n t a l R e s e a r /media/ces/AnneFleig_May2010_CES.pdf
  • 46. 2010_017

    mparing th . The MM onths as sh t areas of t bias. The d n melting o watershed. M5 data above the unoff are t istilfirði (vh Aug Sep O 7.5 4.3 1 7.1 3.9 0 0.4 0.4 0 ure 1961–2 is shown w tures data w erature dat e MM5 tem 5 temperat own in Tab he Austari- ifference is nly takes p As the ele will only c melt thres herefore m m 26), 196 ct Nov Dec .2 -1.7 -3.1 .5 -2.5 -4.1 .7 0.8 1.0 005 for Sa /media/ces/2010_017.pdf
  • 47. ces-glacier-scaling-memo2009-01

    =Sa for DVa >= 0 in case of an advance when there is insufficient space to advance the ice margin. The mean altitude of the ice-covered part of each elevation band or grid cell at the end of the hydrological year is then given as yi +Dha. The increased ice thickness in case DVa >= 0 and there is insufficient space to advance the ice margin is not consistent with the volume–area scaling and needs /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 48. VI_2020_011_en

    Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 49. Factsheet_Bardarbunga_140908

    with underling respiratory problems might be affected although others should not experience any significant discomfort. o Efforts to increase the gas monitoring in inhabited areas are on-going, by The Environment Agency of Iceland. o If eruptive activity continues at similar rates, the air quality in Eastern part of Iceland, will remain similar.  Air quality at the eruption site: o Gas /media/jar/Factsheet_Bardarbunga_140908.pdf
  • 50. Reading material for the PhD Workshop

    -public-good-games Core Partners Finnish Meteorological Institute (FMI /nonam/adaption/material/

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