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  • 41. VI_2014_001

    flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
  • 42. VI_2015_009

    flood models 1–24 (Eqs. 8 and 9 applied with variables 1–12). Ratio between esti- mated and reference index flood (solid black line). The solid blue line corresponds to the reference index flood (Ratio=1), estimated as the arithmetic mean of the observed AMF sample and the dashed blue lines the 95% CI derived from the GEV distribution. Large red symbol indicates overall best model. 18 4.2.2 Flood /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 43. “The small eruption” in

    This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months
  • 44. “The small eruption” in

    This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/
  • 45. Rockslide in Askja, July 21 2014 - Preliminary results of observations

    plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which means that the failure surface /avalanches/articles/nr/2929
  • 46. VI_2014_005

    lines). Additionally, the aver- age profiles for offshore distances to the coast of up to 30 km are shown by the black lines. For temperature, the dashed lines indicate linear projection from the two lowest model levels to 2 m above ground. A comparison of monthly averages of simulated 2-m temperature with station measurements, both for SURFEX and projected values, is shown in Figure 8. On average /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 47. VI_2020_004

    vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 48. VI_2013_008

    on the use of analogues. Analogue-based methods have been used with success in streamflow forecasting. They are often referred to as nearest-neighbor methods (Karlsson & Yakowitz, 1987; Galeati, 1990; Akbari et al., 2011). The first step of the technique is to compare a current situation to all past situations collected in an historical archive, according to a set of attributes describing /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
  • 49. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    the body of knowledge in any given area by mapping out cause-and-effect relationships among key variables and encoding them with numbers that represent the extent to which one variable is likely to affect another (Jensen, 2002). Factors, associations and probabilities can be adjusted and validated and BNs are powerful for integrating data and knowledge from different sources and domains, e.g /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 50. A minor eruption underway

    for the aviation.Reykjanesbraut – the main road from the capital region to Reykjanesbær and the international airport at Keflavík is open. However, Suðurstrandarvegur – the road along the south coastline of Reykjanes peninsula is closed between the two coastal towns Grindavík and Þorlákshöfn. Other roads and unpaved tracks in the close vicinity of the eruption site are also closed.Updated 19.03 23:20At around 20:45 UTC today /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

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