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• 1. Veðurstöðvar

  Veðurstöðvar Alphabetic order Regional order Simple list Aðalvík (xf) I Akrafjall (sj) O I /weather/stations/

• 2. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 3. Group5-Milestones

  Revised catalogue of measures Decision-making 2 Published catalogue of measures *Objective Verifiable Indicators: the quantitative, qualitative, and time-bound measures that constitute evidence of the extent to which the aims have been met (see LogFrame matrix) 2 o Figur 1. Stakeholder participation stage o o When you integrate knowledge from different stakeholders, whose knowledge /media/loftslag/Group5-Milestones.pdf

• 4. Horsens_breakout_12August

  students. If necessary we can form more than one group for the same topic. 2 Group 1 – Scenarios Objective  To build scenarios for use in a 20 years planning process aiming at design of a climate change adaptation plan. Tasks – questions to be answered 1. Knowledge gathering – climate change effects o Which knowledge is needed regarding climate effects and the involved uncertainties? What /media/loftslag/Horsens_breakout_12August.pdf

• 5. IMO_AnnualReport2014

  closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses Increased /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 6. Guidelines2-for-rapporteurs

  Perrels)  For each session report: o start with a heading indicating session number and title o for each presentation: name of presenter(s) and title o start for each presentation summary on a new page  Try to summarize briefly the main lines of argument as well as the project results and conclusions. This can be just like a not too long bullet list. When relevant, you can notify links /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 7. Hare-2011-ParticipatoryModelling

  support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 8. Factsheet_Bardarbunga_140908

  Conclusions of the Scientific Advisory Board of the Icelandic Civil Protection:  The eruptive activity at Holuhraun continues at similar intensity. o The eruption sites are the same as before. Lava flows to the East at similar rates as yesterday. Although the lava is now in contact with the river Jökulsá á Fjöllum, it does not reduce the lava flow rates significantly. No explosive activity /media/jar/Factsheet_Bardarbunga_140908.pdf

• 9. VED_AnnualReport-2013_screen

  Annual report  ? Icelandic Met O?e  Bústaðavegur –  Reykjavík Iceland Editors: Sigurlaug Gunnlaugsdóttir Sigrún Karlsdóttir Ingvar Kristinsson Theódór F. Hervarsson Design and layout: Vinnustofa Atla Hilmarssonar Printing: Oddi Cover photo: Oddur Sigurðsson ISSN - The Icelandic Meteorological O?ce, IMO, is responsi - ble for real-time monitoring and forecasting /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 10. Factsheet-Bardarbunga-140906

  at Bárðarbunga was measured with the radar system of Isavia’s aircraft. The measurements show large changes on the ice-surface. Up to 15 m subsidence has occurred in the centre of the caldera, which corresponds to a volume change of 0.25 km3. The shape of the subsidence area is in accordance with the elevation of the caldera floor having lowered by that amount. o Subsidence of this order has /media/jar/Factsheet-Bardarbunga-140906.pdf