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• 41. VI_2020_011_en

  Erupted lava can have further interactions with water, such as by flowing into the sea where toxic gases can be released or interacting with ground water, a lake or a river. 21 Figure 5: Event tree for the Vestmannaeyjar volcanic system, with the pathways encom- passing the behavior exhibited by the 1973 Eldfell and 1963–1967 Surtsey eruptions indicated. The blue dots indicating “clone /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 42. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 43. Öræfajökull – frequent questions & answers

  the volcano. Question: Should an eruption occur, where from the glacier can the jökulhlaup be expected?Answer: It depends on the location and type of the eruption. Three types of glacial outbursts can be thought about:Floods resulting from an eruption in the caldera, where the ice is up to 500 m thick. Large eruptions can melt of order 100,000 m3/s. Jökulhlaups can be expected from Virkisjökull /volcanoes/about-volcanoes/oraefajokull/q-a/

• 44. CES_D2.4_task1

  NO +58:17:03 +06:38:58 5 P 2662 BJORHEIM I RYFYLKE NO +59:04:39 +06:01:12 64 P 2663 EGERSUND NO +58:27:10 +06:00:11 4 P 2664 HOGNESTAD NO +58:41:40 +05:38:30 19 P 2665 HUNDSEID I VIKEDAL NO +59:33:20 +05:59:44 159 P 2667 LYSEBOTN NO +59:03:24 +06:38:57 9 P 2668 MAUDAL /media/ces/CES_D2.4_task1.pdf

• 45. Bardarbunga_kafli20140825

  could emit >5 km3 of basaltic tephra, covering >50,000 km2 on land. Heavy tephra fall and darkness in proximal and medial areas (<100 km) can be expected (Figure 5b). Tephra fall could reach mainland Europe. Eruptions elsewhere on the fissure swarm will be predominantly effusive and could release 1 - 4 km3 of lava and significant amounts of tephra. Lava can extend tens of km from source, e.g /media/jar/Bardarbunga_kafli20140825.pdf

• 46. Paper-Olafur-Rognvaldsson_92

  is defined as a 24 hour period where the simulations are dry (rmm5 ≤ 0.1) but the observations are wet (robs > 0.1). Figure 5 shows the percentage of missing events during the summer months (JJA) at each of the observation stations. There is higher probability of missing events during sum- mer than in winter (map not shown). In Fig. 6 the precipitation during missing Figure 3: Ratio [%] of "false alarms /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 47. 2010_017

  be expected by rain, incoming groundwater flow, and snow and ice melt. The source of this excess water was traced to the glacier. Under normal circumstances the groundwater level is calculated in two modules in WaSiM: i) in the module for the unsaturated zone where the groundwater level is estimated from infiltration and the release of groundwater as spring flow, and ii) in the groundwater module /media/ces/2010_017.pdf

• 48. 2010_003rs

  as large green stars in boxes O and N respectively. The epicentre of the 29 May 2008 earthquake is also marked in box I. The four smaller green stars show the hypocentres of four M~5 earthquakes, triggered by the J17 event. The study area was divided into fifteen boxes, outlined on the map and marked by A-O, for analysis. Roughly half of the nineteen thousand events displayed here, occurred outside /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 49. VI_2020_004

  %. An eruption like 1918 at Katla would have an intermediate impact on the ground where several inhabited or touristic areas, such as Þórsmörk, Vík, Landmannalaugar Skógar, could be affected by a fallout greater than 100 kg/m2 (~10 cm). No part of the road system falls into the category of high probability (>75%) for critical driving conditions. However, more than 150 km can may fall /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 50. CES_BioFuels_Flyer_new

  and how future climate change within the next 20–30 years can impact these resources. In the future, an increase in the utilization of various sources of bioenergy will increase in Nordic countries. This raises a question what is the biomass production potential of forests now and in the future and how sustainable the energy production based on biomass are owing to possible large-scale harvestings /media/ces/CES_BioFuels_Flyer_new.pdf