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Results:

• 11. IPPC-2007-ar4_syr

  the respective WG reports. Unless otherwise stated, numerical ranges given in square brackets in this report indicate 90% uncertainty intervals (i.e. there is an estimated 5% likelihood that the value could be above the range given in square brackets and 5% likelihood that the value could be below that range). Uncertainty intervals are not necessarily symmetric around the best estimate. 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 12. RaisanenJouni_CES_2010

  increases by 2.1ºC, and the interannual standard deviation dec- reases by 6%, when the simulated global mean T increases by 1ºC. Of course, there is variation between different models! Time series of winter mean temperature in Helsinki (1961-2008) Blue line = observations Red line = best-estimate present-day (2010) climate Grey dots = results for individual models Probability distribution /media/ces/RaisanenJouni_CES_2010.pdf

• 13. Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland

  inundations, in a context where experience of past floods is the best predictor of awareness. /media/loftslag/Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland.pdf

• 14. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 15. raisanen_ruosteenoja_CES_D2.2

  ............................................................................................................ 4 3. Best estimates of temperature and precipitation change................................................ 7 4. How certainly will temperature and precipitation increase? ....................................... 10 5. Uncertainty ranges and quantiles of temperature and precipitation change .............. 12 6. Hindcast verification of the resampling ensemble /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 16. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 17. VI_2014_005

  temperature and wind speed over terrain below 100 m above mean sea level (mASL) (see Figure 4), model grid-points below that level are ignored for the calculation of best linear fits of vertical profiles. Terrain-following gradients obtained for 2-m air temperature are -6.0 K km 1 in January, and -7.2 K km 1 July. For 10-m wind speed, the terrain-following gradients are 3.4 m s 1 km 1 in January /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 18. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  that learning to improve the next stage of management (Holling, 1978). AM treats policies and management interventions as experimental probes designed to learn more about the system; they are not confident prescriptions (Lee, 1993). Monitoring before and during the intervention, enables the system response to be determined and thereby allows managers to learn from past experience and to translate the best /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 19. Awards and press

  Asked what they liked best about the web-site, most mentioned some of the following: Clarity and graphical presentation of weather Earthquake information in addition to weather Quantity of information and knowledge Just over 60% claimed to use this web every day and about 90% daily or a few times a week. General satisfaction neither depends on age, region nor pattern /about-imo/the-web/awards_and_press/

• 20. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf