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• 11. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 12. norsem_ragnar

  From the Nordic SIL research project towards warnings on the long- and on the short-term before large earthquakes Ragnar Stefánsson University of Akureyri From it´s start in 1988 the SIL project was based on physical approach in earthquake prediction research. It was also stated from the start that the best information about crustal processes preceding earthquakes would come from /media/norsem/norsem_ragnar.pdf

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

  can be found in Huntjens et al. (2007), Chapter 4 of NeWater Deliverable 1.7.9a (http://www.newater.info). Climate change adaptation in European river basins 265 123 interactions, by private and public actors, to achieve adaptation and to enhance the capacity of processes, institutional arrangements and actors to adapt to future environmental changes (Huitema et al. 2009). Adaptive governance /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 14. Hare_1_PartINONAM

  Participatory methods and processes for adaptive management Dr Matt Hare Independent Consultant, Mexico City Adaptive and participatory water management Matt Hare, hare@gmx.de 2011 – Summer School About myself ... • Bachelor in artificial intelligence (88-92) • PhD environmental modelling in knowledge and data-poor domains (95-99) • Co-founder of Seeconsult GmbH (03-onwards /media/loftslag/Hare_1_PartINONAM.pdf

• 15. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 16. Safetravel in winter

  night and day, all year round. 112 Iceland app Safetravel provides 112 Iceland, an app which is easy to use. It can be used in emergency, if an accident occurs or if someone is lost. Tourist can also leave their "trail" in case of search. From Safetravel's web-site, the app can be downloaded for either Android phones, Windows phones or iPhone: First of all you can call for help by pressing /about-imo/news/nr/3220

• 17. Landslides

  is usually easily eroded. If the mass is big enough, the momentum and speed can become sufficiently large to snatch up bridges, buildings or other infrastructure and therefore cause large amount of damages. One of the most infamous hazard caused by lahars occurred after the eruption in Pinatubo in 1991. https://pubs.usgs.gov/fs/1997/fs114-97/ Another example is the devastating lahar /volcanoes/volcanic-hazards/landslides/

• 18. Lava flows

  in Heimaey in 1973. Heimaey is in the Vestmannaeyjar Archipelago west of Iceland and it lies within an active volcanic zone. During the eruption of 1973 a part of the town was submerged by the lava and the sailing routes to the harbour was almost closed off because of the lava flow. A world known operation to cool the advancing lava with sea water saved the harbor. Largest flood /volcanoes/volcanic-hazards/lava-flow/

• 19. Bárðarbunga earthquakes 3D

  of earthquakes in Bárðarbunga 16 - 26 August 2014. IMO's specialist, Bogi B. Björnsson, compiled this video from the available data. 16 - 20 August 2014 The Bárðarbunga seismic activity can now be explored in a three dimensional video (30 sec.) which shows earthquakes from 16th to 20th August 2014. Location, depth and age of earthquakes in Bárðarbunga 16-20 August 2014. The colour /earthquakes-and-volcanism/articles/nr/2948

• 20. Eyjafjallajokull_status_2010-06-07_IES_IMO

  June. In the western part of the crater, a new crater has formed at the site of explosive activity. Tremor pulses late 6 June accompanied steam plumes from this new crater. The plumes and explosions are small. Caving in of lava in the conduit can be heard between explosions. Only a part of the new active crater has been seen due to the steam. The glacial ice at the top is advancing rapidly /media/jar/Eyjafjallajokull_status_2010-06-07_IES_IMO.pdf