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• 41. 2010_003rs

  ........................................................ 19 2.3.2 Changing the maximum number of events in a group ................................. 20 2.3.3 Rearrange order of input .............................................................................. 22 2.3.4 Relocate only the best events ....................................................................... 22 2.3.5 Other tests /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 42. IPPC-2007-ar4_syr

  of about 29,000 data series was selected from about 80,000 data series from 577 studies. These met the following criteria: (1) ending in 1990 or later; (2) spanning a period of at least 20 years; and (3) showing a significant change in either direction, as assessed in individual studies. These data series are from about 75 studies (of which about 70 are new since the TAR) and contain about 29,000 data /media/loftslag/IPPC-2007-ar4_syr.pdf

• 43. VI_2009_006_tt

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 3.4 Cumulative volume of floodwater from the Skaftá cauldrons. . . . . . 16 3.5 Discharge in the 2006 and 2008 jökulhlaups from the Western Skaftá cauldron. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 3.6 A transect of the subglacial path of jökulhlaups from the Eastern Skaftá cauldron and the glacier surface. . . . . . . . . . . . . . . . . . . . . 20 3.7 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 44. Markarfljót outwash plain and Öræfajökull

  to the local readership. Release of the Icelandic version is scheduled in March/April 2016. Downloadable material: Full text (pdf 23 Mb) Front matter (pdf 180 Kb) Table of contents (pdf 7.9 Kb) Chapter I. Volcanogenic floods in Iceland: An exploration of hazards and risks (pdf 1.06 Mb) Pages 7–16 Emmanuel Pagneux, Sigrún Karlsdóttir, Magnús T. Gudmundsson, Matthew J /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 45. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 46. The weather in Iceland in 2021

  and early summer was cold, dry and sunny. Towards the end of June, it warmed up quickly especially in the North and East with maximum temperatures well above 20°C in many places for several days. The sudden warm weather, after the cold spring, caused a rapid snow melt in the mountains, increased runoff and extensive flooding in major rivers and streams. This exceptionally warm weather /about-imo/news/the-weather-in-iceland-in-2021

• 47. Tornado_Impacts_-_FMI_Presentation

  office to construct a Doppler radar treatment variable. introduced; also measures of tornado warnings improved. In current analysis with additional control variables and more years of data we find 30% and 44% reductions in fatalities and injuries. Warnings and Casualties 100 120 140 160 180 I n d e x V a l u e Fatalities 0 20 40 60 80 NoWarning Lead1-5 Lead6-10 Lead11-15 Lead16-20 /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf

• 48. Grimsvotn_status_2010-11-01_IES_IMO

  this morning gave 455 m3/s, and another measurement, around 16:00 GMT, showed an increase to 627 m3/s. Electrical conductivity has increased since the beginning of the outburst from 180 µS/cm to 320 µS/cm. Seismic tremor: Seismic tremor has been increasing at seismic station ‘grf’, located near Grímsvötn, since late on 27 October 2010. This tremor is similar in character to the tremor /media/vatnafar/flod/Grimsvotn_status_2010-11-01_IES_IMO.pdf

• 49. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/

• 50. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera