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Results:

• 21. event_numbers_31102014_1900

  Earthquakes between 16. August 2014 00:00 and 31. October 2014 19:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 28.000 - - - - - - - checked ~ 11.900 ~ 6.500 ~ 3.550 ~ 140 ~ 260 ~ 1.200 ~ 250 ~15 M3.0-3.9 434 99 321 6 2 3 2 1 M4.0-4.9 228 7 219 1 1 0 0 0 M>5.0 61 0 61 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll /media/jar/event_numbers_31102014_1900.pdf

• 22. Guidelines2-for-rapporteurs

  Adaptation conference 29-31 August 2012 – Helsinki – Rantapuisto Guidelines for rapporteurs  Please report the sessions assigned to you (see table below)  You can swap sessions with another rapporteur, if the concerned rapporteur explicitly affirmed that swap and no other time or task conflicts occur (this is to be checked with the co-chair who coordinates rapporteur slots – Adriaan /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 23. Instructions on using wind, precipitation and temperature forecasts

  The colours represent 2°C temperature intervals. The temperature scale on the image changes according to the temperature range of the forecast. Wind forecasts: The map displays wind direction and wind speed (in m/s) based on 10-minute averages. Wind direction is denoted by arrows. The wind-speed scale on the image changes in relation to the forecast speed. The lowest wind /weather/articles/nr/1211

• 24. Snow avalanche stopped by a catching dam

  in a gully below a shelf in the middle of the mountainside at approximately 340 m a.s.l. It flowed down the gully and onto a road above a recently constructed catching dam which is a short distance above the uppermost houses in the village. The avalanche hit the dam along a more than 50 m distance and left rocks and branches that it picked up on its way on the damside. It was approximately 2 m short /about-imo/news/nr/3041

• 25. 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

• 26. Group5-Stakeholders_involvement

  /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf

• 27. Linnet_Ulfar_CES_2010

  HYDROPOWER IN ICELAND Impacts and adaption in future climate Authors Óli Grétar Blöndal Sveinsson (Phd) Úlfar Linnet (MSc) Elías B. Elíasson (MSc) Landsvirkjuns system •Installed power 1850 MW • 96 % Hydroelectricity • 4% Geothermal •Production capacity 13 TWh/a •Customer base • 86 % Large industries • 14 % Small businesses / Household •No connection to other countries •Reliability a major /media/ces/Linnet_Ulfar_CES_2010.pdf

• 28. 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

• 29. Strong gales

  9th, lasting well into Saturday morning. Wind speeds measuring 20 m/s and higher were recorded at half of the automatic weather stations in the lowland areas and similar speeds were recorded at 80% of automatic weather stations in the highland areas. In the town of Heimaey in the Westman Islands, wind-speed* of 28 m/s and gusts measuring 45.8 m/s were recorded at the height of the storm, setting /about-imo/news/nr/1732

• 30. Strong gales

  A great storm passed over Iceland on Friday night, October 9th, lasting well into Saturday morning. Wind speeds measuring 20 m/s and higher were recorded at half of the automatic weather stations in the lowland areas and similar speeds were recorded at 80% of automatic weather stations in the highland areas. In the town of Heimaey in the Westman Islands, wind-speed* of 28 m/s /about-imo/news/nr/1732/