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Results:

• 41. VI_2013_008

  ll l l l l l l l l l l l l ll l ll l l l l l l l l l ll l l l l l l l l lll l l l l l l l l ll ll l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l ll l l ll ll l l l l l l ll l l l l l ll l l ll l l l l l l l ll l ll ll l l l l 0 500 1000 1500 50 0 100 0 150 0 Prediction (m^3/s) O bs . (m ^3 /s) vhm 64 Method 1 T+2 llll ll ll llllllll l l ll l lll l l l l lll l l l ll l l /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 42. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  2004 after finishing the case study. Newspapers were distributed to 1000 households in the local area. At the final joint meeting where both groups participated in March 2004 (step 7), the stakeholder groups were asked to comment on the involvement process on the basis of four questions: (1) Is there a need for further initiatives for the protection of groundwater? (2) How have you experienced /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 43. A minor eruption underway

  earthquakes were detected. Three were larger than magnitude 3, the largest M3.3 at 2:37AM located around 1km N of Nátthagi valley. Today at 13:00GMT the Scientific Advisory Board of the Icelandic Civil Protection will meet to evaluate the latest monitoring data. Findings of the meeting are expected shortly after 15:00GMT.Updated 15.03 at 11:00 Since midnight over 1000 earthquakes have been detected /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 44. Information and help

  a truck; destroy a small building or break a few trees. 1000 tonn 4 Could bury and destroy a railway car, large truck, several buildings or a piece of forest. 10.000 tonn 5 Could gouge the landscape; disastrous damage potential. 100.000 tonn It is not always easy or obvious how to classify the size of an avalanche, however, the destructive potential is the predominant /avalanches/forecast/help

• 45. VI_2019_009

  layer from station level (not sea level), in ascending order that correspond to the intervals 0-50m, 50-100m, 100-200m, 200-300m, 300-600m, 600-1000m, 1000-1500m, 1500-2000m, 2000-2500m and >2500m and if the height is between intervals, it’s rounded up. Mountains are typically used to estimate the height of the clouds, if that’s not possible the type of clouds are studied to estimate the height /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 46. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 47. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 48. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  ; (1) where N is the number of years between the elevation maps, A1 is the average area (m2) of the ice cap over N years, r is the scaling factor from the density of ice (900 kg m3) to water (1000 kg m3), DV D ¯hA2; (2) is the total volume loss (m3), D ¯h is the N year area- average elevation change (m) for the whole ice cap and A2 is the maximum area (m2) of the ice cap. In this study we use /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 49. Bárðarbunga 2015 - February events

  Sciences, 17 - 19 February: There is only one active vent inside the crater and the surface of the molten lava continues to sink. The lava channel has crusted over, except the 200 - 300 m nearest to the vent. The eruption column reaches no more than 1000 m above ground. The photos below show breakouts 15 – 16 km ENE of the vent, fed by the closed lava pathway which is inflating the lava field /earthquakes-and-volcanism/articles/nr/3087

• 50. Bárðarbunga 2015 - February events

  Sciences, 17 - 19 February: There is only one active vent inside the crater and the surface of the molten lava continues to sink. The lava channel has crusted over, except the 200 - 300 m nearest to the vent. The eruption column reaches no more than 1000 m above ground. The photos below show breakouts 15 – 16 km ENE of the vent, fed by the closed lava pathway which is inflating the lava field /earthquakes-and-volcanism/articles/nr/3087/