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• 51. VI_2020_004

  ....................................................................................................................................... 9 Ágrip ......................................................................................................................................... 11 1 General introduction ........................................................................................................... 13 1.1 Main aim of the project /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 52. Hofsjökull ice cap gains mass

  and Drangajökull ice caps. All ice caps in Iceland have been retreating rapidly and losing volume since 1995, but in 2015 the Hofsjökull ice cap in the central highlands displayed positive mass balance. The equilibrium line altitude on the ice cap moved to a location 150 - 200 below the long-term average. This change is due to high precipitation in the winter of 2014 - 2015 and low ablation /about-imo/news/nr/3229

• 53. 2010-05-02_En-IES_IMO

  the eruption site. Plume track visible at least 200 km from the eruption site on MODIS (12:35 GMT) and EUMETSAT (17:15 GMT) satellite imagery. Colour: Dark grey (ash) clouds observed over the eruptive site. White (steam) plumes rising from Gígjökull, north of the eruption site. Tephra fallout: Moderate ash-fall reported in the village of Vík (12:00 GMT), located 40 km south-east /media/jar/2010-05-02_En-IES_IMO.pdf

• 54. Eyjafjallajokull_status_2010-04-30_IES_IMO

  :00 GMT a flood was detected leaving the Gígjökull lake basin. The flood reached a maximum discharge about two hours later at the old bridge over Markarfljót, ~18 km downstream. The flood was comparable in size to yesterday's gauged flows. At 14:00 GMT, meltwater flow beneath the bridge was ~200 m3 s–1. Discharge from Gígjökull decreased during the afternoon. Steaming blocks /media/jar/Eyjafjallajokull_status_2010-04-30_IES_IMO.pdf

• 55. Refsgaard_etal-2007-Uncertainty-EMS

  : Integrated water resources management; Water framework directive; Catchment modelling; Uncertainty 1. Introduction New guidelines on water resources management emphasise the importance of integrated approaches, cross-sectoral plan- ning and of public participation (GWP, 2000; EC, 2003; Jønch-Clausen, 2004). The commonly accepted approach inte- grated water resources management (IWRM) is defined /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 56. The weather in Iceland 2014

  above the 1961 to 1990 average. It was also the second warmest year in Akureyri (since the start of the series in 1881), only 1933 was warmer. The temperature was far above normal until October. Reykjavík blue, Akureyri red. November was also extraordinarily warm, but December considerably colder and the coldest month of the year. Table 1. Temperature in 2014 station temp °C dev. 1961-1990 /about-imo/news/nr/3082

• 57. ved-eng-2014

  month of the year. Table 1. Temperature in 2014 station temp °C dev. 1961-1990 rank of dev. 2004-2013 Reykjavík 6.0 1.7 2 144 0.6 Stykkishólmur 5.3 1.8 3 169 0.6 Bolungarvík 4.7 1.7 5 117 0.7 Bergstaðir 4.7 2 37 0.9 Grímsey 4.9 1 141 1.3 Akureyri 5.3 2.1 2 133 1.0 Grímsstaðir 2.8 2.3 1 108 1.3 Egilsstaðir 5.1 2.2 1 60 1.3 Dalatangi 5.3 1.9 1 76 0.7 Teigarhorn /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 58. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  su lta tio n o f st ak eh ol de rs, co m m en tin g an d o bje cti ng o n go al s an d tra ns bo un da ry as pe ct s (Ens erin k et al .200 3; Raa dgeve ran d Mos ter t200 5). Asse ssmen to fexi stin g situatio n D at a (na tu ra ls ys te m s): 1: Ep ist em ic O fte n do m in an t In te rn at io na lm o n ito rin g n et w or k se tu p, i.e .thr oug h IC PR .Su stainabl e tra ns bo un da ry co o pe /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 59. Re-evaluation needed of the size of the hazard area

  Oddsson/Department of Civil Protection and Emergency ManagementUpdated 05.04 at 14:15A new additional fissure opened at ca. 12:00 hrs today near the initial eruption site in Geldingadalir. First estimates of the length of the fissure is ca. 200 meters, and the middle of the fissure is approximately 1 kilometer NE of the eruption site in Geldingadalir. The lava from the new fissure flows toward /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 60. VI_2014_006

  0 0 20 12 % Grassland <1 43 25 10 25 % Woodland <1 0 0 2 2 % Moss 59 25 0 14 13 % Little or no vegetation 35 27 30 63 36 % Wetland 0 5 46 6 7 % Lakes 6 <1 <1 <1 3 300 400 500 600 700 800 30 0 40 0 50 0 60 0 70 0 km km 2400 2200 2000 1800 1600 1400 1200 1000 800 600 400 200 0 m.a.s.l Watershed Glacier vhm19 vhm10 vhm26 vhm64 vhm66 Figure 1. Topography of Iceland and location of the watersheds /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf