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Results:

• 21. CES_D2.4_solar_CMIP3

  (an average of 18 mod- els) is depicted in Figs. 3 (in percentage terms) and 4 (in absolute terms). In the relative sense, largest changes occur in winter in central Scandinavia and southern Finland, where more than 5% of incident radiation would be lost (Fig. 3(a)). According to the t test, the signal is statistically significant at the 1% level. Over the Barents Sea, the decline is even larger /media/ces/CES_D2.4_solar_CMIP3.pdf

• 22. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 23. ces-glacier-scaling-memo2009-01

  advance is only crudely modelled. The main features of the model are Glaciers within the modelled watershed are divided into one or more groups that are treated together more or less as one ice body each in the simplified glaciological mod- elling. The total ice volume is separately estimated for each group of glaciers so that the runoff from the corresponding glaciated part of the watershed /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 24. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 25. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 26. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 27. ces_geus_paakitsoq_full_report

  at Il- lulisat and Station 437 compared to standard deviation of Ta mod- elled by RCAO for the corresponding RCM grid-boxes. (b) The same for the stations Swiss Camp and Crawford. (c and d) The same as plot a and b, respectively, but for HIRHAM4. summer (Fig. 6a). Parameterized Sin has only a small negative bias during summer (Fig. 6b). Standard deviation of monthly means is similar /media/ces/ces_geus_paakitsoq_full_report.pdf

• 28. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 29. IMO_AnnualReport2014

  of events 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 /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 30. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf