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Results:

• 21. VI_2022_006_extreme

  is the RCP 8.5, in which greenhouse gas concentrations will continue to rise. This scenario is often used as the worst-case scenario, if nothing is done to reduce the emissions. A subset for both scenarios is archived at the IMO and is available for a large domain around Iceland, extending between latitudes 60.5 and 69.5°N and longitudes 10 and 30°W, with a horizontal resolution of 1 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 22. vonKorff_etal-2010

  that they offer general principles and processes that help designers to develop participation processes for unique initial design contexts. This means that they are the opposite of a blueprint, which outlines how a participation process should look. a71 They can be applied to various domains of participation even though the backgrounds of several of their authors are domain-specific. a71 /media/loftslag/vonKorff_etal-2010.pdf

• 23. raisanen_ruosteenoja_CES_D2.2

  concern. However, even if the hindcast methodology were perfectly correct, the observed changes would still be expected to fall outside the 5-95% range on the average in 10% of the domain. Furthermore, in a relatively small area such as that depicted in Figure 5.1, this fraction may vary considerably by chance. The actual area fraction of grid boxes in which the observed temperature changes fall /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 24. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  domain models and are also capable of handling uncertain information in a practical and under- standable way (Jensen, 2002; Henriksen et al., 2004, 2007a, b; Bromley, 2005). BNs have gained a reputation of being powerful techniques for modelling complex problems involving uncertain knowledge and impacts of causes. BNs are a technique which is especially helpful when there is a scarcity and uncertainty /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 25. IMO_AnnualReport2014

  to the measured state of the near-surface atmos- phere. Starting this year, an improved surface cover description will be implemented in the model. In addition, the model domain will be increased. Both changes should result in improved weather forecasts. Icing map. An example of the simulation of in-air icing loads. Projects Weather forecast at the start of the volcanic eruption in the Holuhraun /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 26. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  air, urban zoning, safety etc.), and on the ability of the road transport sector (incl. its infrastructure and supporting services) to co-operate coherently to find efficient and timely answers (Salanne et al, 2010). All in all there are three main domains of effects, being (1) traffic safety, (2) road maintenance, and (3) traffic capacity. Effects in the domain of traffic safety follow from /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 27. VI_2013_008

  these techniques to forecast daily streamflow in Iceland is explored. The method proposed here builds on the different approaches described above and makes use of synoptic meteoro- logical information over a large domain around Iceland and hydrological and meteorological information within the catchments of interest to forecast daily streamflow up to 3 days ahead. In Section 2, the principle /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 28. ces-oslo2010_proceedings

  by an objective version of the Hess-Brezowsky Grosswetterlagen (OGWL; James, 2007) modified for the COST733 Action1. The OGWL has been identified as well suited for regional hydrological drought studies in north-western Europe (Fleig et al., in press 2). It is derived on a domain covering the eastern North-Atlantic and Europe (30°-76°N; 37°W-58°E) and yields 29 WTs. The WTs are characterised /media/ces/ces-oslo2010_proceedings.pdf

• 29. Adalgeirsdottir-etal-tc-5-961-2011

  the location of the mass balance stakes at Breiðamerkurjökull (Bre). The red box indicates the posi- tion of the frame to the right. (C) Hoffellsjökull surface topography in 2001. The ice divide and the model domain are indicated with the red curve enclosing a glaciated area of ∼212 km2 in 2001. Black triangles show the locations of automatic weather stations on the glacier. N is the location /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 30. Bárðarbunga 2014 - October events

  on observations in the field 2 and 4 October, but also on a radar image since 30 September. Since then, the southernmost tongue has advanced 3 km NA parallel to earlier lava streams. The lava field has broadened somewhat towards south. Enlarge. Institute of Earth Sciences. Domain From the field, 4 October 2014. The new and sizzling hot lava forces the glacial river Jökulsá á Fjöllum eastwards /earthquakes-and-volcanism/articles/nr/3011