Search

83 results were found for Sökmotor Android 🔍 www.46.gg.


Results:

  • 61. Horsens_case

    NONAM Summerschool Copenhagen 22-26 August 2011 1 HORSENS FJORD CASE Hans Jørgen Henriksen, GEUS 1. Background to the case Introducing the catchment Horsens Fjord is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1). The surface area of the Fjord is approximately 46 km2 and the mean depth is 2.9 m besides /media/loftslag/Horsens_case.pdf
  • 62. VI_2020_004

    ............................................................................ 44 Figure 19 Probabilistic hazard map for a tephra load ≥0.1 kg/m2 (Hekla) ............................. 45 Figure 20 Probabilistic hazard map for a tephra load ≥10 kg/m2 (Hekla) .............................. 46 Figure 21 Probabilistic hazard map for a tephra load ≥100 kg/m2 (Hekla) ............................ 47 Figure 22 Seasonal analysis of tephra load probability exceeding 0.1 kg/m2 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 63. GA_2009_91A_4_Andreassen

  • 64. Eriksson_Garvill_Nordlund_2006

    ) measures. The main purpose ARTICLE IN PRESS of this study is to test a model of the relations between factors expected to influence the acceptability of TDM measures. In addition, comparisons between car users’ 0272-4944/$ - see front matter r 2006 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvp.2006.05.003 Corresponding author. Department of Psychology, Umea˚ University, Sweden. Tel.: +46 90 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 65. Kok_et_al._TFSC_published_2011

  • 66. Lorenzoni_Pidgeon_2006

    %) and man-made disasters (46%). However, significant differences were evident between responses in the former EU-15 and the newer 10 MS. On average, climate change was the most mentioned environmental concern in the EU-15 (47%), whereas it was only mentioned by 34% of respondents in the newer 10 MS (e.g. 28% in Latvia, 32% in Hungary but 43% in the Czech Republic). This average is below the lowest /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 67. Refsgaard_etal-2007-Uncertainty-EMS

  • 68. VI_2009_006_tt

    in the underlying subglacial lake. . . . . . . . . . 39 5.3 The hypsometric curve for the subglacial lake below the Western Skaftá cauldron. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45 5.4 Temperature at the bottom of the subglacial lake under the Western Skaftá cauldron. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 46 5.5 Temperature in river Skaftá at Fagrihvammur during /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 69. VI2010-006_web

    tímabilið 1949–2009. T P1d P2d P3d P5d 1 22 29 35 43 2 26 35 41 51 5 32 43 50 61 10 36 49 56 68 20 40 55 62 75 50 46 62 71 85 og 5 daga tímabil fyrir veðurstöðina á Akureyri. Taflan sýnir úrkomu sem svarar til 1, 2, 5, 10, 20 og 50 ára endurkomutíma, þ.e. tölfræðileg greining bendir til að úrkoma verði ekki meiri en sem nemur gildunum í töflunni oftar en endurkomutíminn segir til um þegar til langs /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
  • 70. Bárðarbunga 2014 - September events

    its way parallel to other flows. Therefore, the combined surface area of the lava field is no less than 46 km2. 29 September 2014 11:30 - from the Scientific Advisory Board Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland along with representatives from the Icelandic Civil Protection and the Directorate of Health. From the Scientific /earthquakes-and-volcanism/articles/nr/3001

Page 7 of 9






Other related web sites


This website is built with Eplica CMS