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  • 51. VI_2020_011_en

    Grain size distribution from heimaey 1973 eruption ..................................................... …64 D. Age of vents relative to best fit line ............................................................................... …65 E. Weight-bearing capacity of homes in heimaey .............................................................. …67 F. How to contextualize the probabilities given /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 52. hafisskyrsla_11052011

    ísrandarinnar, sem og myndir úr eftirlitsratsjá og kort sem unnið var á SLAR ratsjánna. Á neðangreindri töflu sést lega íssins frá sv-na. 1. 67 22N 026 13W 2. 67 26N 025 23W 3. 67 38N 025 28W 4. 67 46N 025 00W 5. 67 40N 024 46W 6. 67 41N 024 02W 7. 68 02N 023 30W 8. 68 07N 023 03W 9. 68 21N 022 30W 10. 68 32N 022 08W 11. 68 26N 021 41W 12. 68 40N 020 44W 13. 68 47N 020 05W 14. 69 10N /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf
  • 53. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    tgovernmen tbodie s ar e involve d in settin g th e TOR s an d supervisin g th e search ,o r at leas tconsulte d (interviews ,survey s etc. ) Dub e an d Swatu k (200 2) Ide m fo rnon-governmenta lstakeholder s (e.g .environmenta lNGO’s ,use r groups ,citize n group s o r privat e sector ) Brannstro m et al .( 200 4), Sumber g an d Okal i( 200 6), Huisma n et al .( 200 0), Mart y (200 1) 19 /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 54. A minor eruption underway

    of gas pollution. The latest gas dispersion forecast is accessible at the top of the IMO website, en.vedur.is. Updated 20.03 13:45What we know so farAt around 20:45 UTC 19 March 2021, a volcanic eruption began at Geldingadalur, close to Fagradalsfjall on the Reykjanes Peninsula. The eruption was first seen on a web camera positioned close the mountain. It was also confirmed on thermal satellite /about-imo/news/earthquake-swarm-in-reykjanes-peninsula
  • 55. VED_AnnualReport-2013_screen

    air pressure, solar radiation and cloud cover, as well as time-series on hydrology, glaciology, earthquakes, floods, sea-ice condition, crustal deformation, avalanches, sediment load in rivers and air pollution. In addition, new fields of re- search and technology are constantly being pursued and developed, e.g. with remote sensing, with the main objective to enhance the capability of IMO /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
  • 56. NOMEK09_Report

    Hermannsdóttir (Media) Sveinn Brynjólfsson (Avalanche) Theodor Freyr Hervarsson (Aviation) Guðrún Nína Petersen (Forecast errors) SMHI: Andreas Carlsson (Dynamics/NWP) Anna Eronn (Satellite) met.no: Bjørn Røsting (Dynamics) FMI: Vesa Nietosvaara (Online sessions and website) Elena Saltikoff (Radar-distans teaching) DMI: Claus Petersen (Slippery Roads) EUMETSAT: Jochen Kerkmann (Satellite /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf
  • 57. Kok_JGEC658_2009

    are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy The potential of Fuzzy Cognitive Maps for semi-quantitative /media/loftslag/Kok_JGEC658_2009.pdf
  • 58. VI_2020_008

    different locations. The results are also presented in map form, both within this report and via a forthcoming website intended for environmental and civil engineers. Note that the website is scheduled for release in 2022; those requiring a digital copy of the revised 1M5 maps should contact IMO via https://www.vedur.is/. The research was funded by Ofanflóðasjóður – Iceland’s National Snow /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 59. CES_D2.4_task1

    SE +59:21:00 +18:03:00 44 P 28 HELSINKI FI +60:10:00 +24:57:00 4 TP 29 JYVASKYLA FI +62:24:00 +25:40:59 137 TP 30 SODANKYLA FI +67:22:00 +26:39:00 179 TP 65 DALATANGI IS +65:16:00 -13:34:59 9 TP 66 REYKJAVIK IS +64:07:59 -21:54:00 52 TP /media/ces/CES_D2.4_task1.pdf
  • 60. ces-oslo2010_proceedings

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