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• 51. FAQ

  on the plume dynamics affecting the final top altitude. Very strong wind can bend the rising mixture causing a lower top altitude and the maximum plume height to be located downwind the eruptive vent. The type and style of the eruption also affect the plume altitude as well as the size of the erupted material. Pyroclastic material in the plume is subjected to two main forces: the force of gravity /volcanoes/grimsvotn-activity/faq/

• 52. 2010_003rs

  by an approximately 70 km long and 15 km wide left lateral shear zone, the South Iceland seismic zone (SISZ). Approximately every 100 years a sequence of large earthquakes of magnitudes M 6-7 occurs in the zone and traces of many Holocene faults have been mapped on the surface. Although the trend of the zone is east-west, major earthquakes take place on north-south striking faults, which leads /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 53. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 54. VI_2009_006_tt

  being the source area for groundwater inflow into the geothermal circulation. If the feeding of the geothermal circulation is from within the watershed of the cauldron, the power to melt the corresponding amount of ice must come from the geothermal area. If on the other hand the feeding is from other areas 10 Figure 3.2: Top: The Skaftá cauldrons on 25 February 1986. View towards east, the west /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 55. Weather stations

  fjordssjObs.ForecastMeteogramInfo.Obs. data Brú á JökuldalE coastalsjObs.ForecastMeteogramInfo.Obs. data Brúarjökull B10CentralsjObs.Info.Obs. data BrúaröræfiCentralsjObs.Info.Obs. data BrúsastaðirNorth WsjObs.ForecastMeteogramInfo.Obs. data BræðratunguvegurSouthsjObs.Info.Obs. data BúlandshöfðiBreiðafjsjObs.Info.Obs. data BúrfellSouthsjObs.ForecastMeteogramInfo.Obs. data Return to the top of the page D DalatangiE /weather/stations/

• 56. Guidelines2-for-rapporteurs

  sessions of the same rapporteur can be put in one document (‘rapporteur_name_session_numbers’)  It is assumed you have an own laptop available. Please notify us in time, in case you cannot bring your own laptop  Make sure the laptop’s battery is charged when you start reporting Link between session reporting and closing session presentation  Obviously the session reports help to prepare /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 57. Milly_etal-2008-Stationarity-dead-Science

  hedged against small climate changes. Additionally, climate projec- tions were not considered credible (12, 14). Recent developments have led us to the opinion that the time has come to move beyond the wait-and-see approach. Pro- jections of runoff changes are bolstered by the recently demonstrated retrodictive skill of cli- mate models. The global pattern of observed annual streamflow trends /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 58. Horsens_case

  in MIKE SHE / MIKE 11 in order to describe climate change effects on groundwater and surface water systems (Fig. 2 and Fig. 3) Figure 2 Regional flow model for catchment area to Horsens Fjord and Norsminde Fjord. The figure also show major highways, main roads and the topography in the area. NONAM Summerschool Copenhagen 22-26 August 2011 3 Figure 3 Zoom in on Horsens by area. Hansted å /media/loftslag/Horsens_case.pdf

• 59. Group-1_Scenarios-for-AWM

  example can be given by the low cost still flood risk adaptation by implementing early warning system. But there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens. Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 2 / 3 R es e a r c h Flood f r equenc y a n d i n t ensi t y c o m m un i c a t /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 60. VI_2009_012

  densely populated farmland containing a few small towns, exposing a few thousand people to the hazards of strong to severe Earth shaking. The WVZ is mostly uninhabited, but the proximity of the capital, Reykjavík, to the WVZ and the SISZ, however subjects tens of thousands of people to moderate effects of shaking. Major power-lines to the capital, telecommunications and roads are also /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf