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Results:

• 11. ces_SA_group_flyer_new

  series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf

• 12. raisanen_ruosteenoja_CES_D2.2

  in Table 2.1. Some potential limitations of using the CMIP3 ensemble for probabilistic climate change forecasting should be mentioned. First, current GCMs still have a relatively coarse horizontal resolution. Within the CMIP3 ensemble, the grid spacing varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude (for the analysis presented here, all the model results were /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 13. 2010_005_

  A more detailed analysis of linear 2004–50 SAT trends as a function of terrain elevation is given in Fig. 5. In the SMHI-RCAO and MetNo-HIRHAM runs, SAT trends increase with height up to about 600 m. Above that elevation and to the top of the terrain, trends remain constant in the SMHI-RCAO, but decrease slightly in the MetNo-HIRHAM. In the DMI-HIRHAM5, warming rates over the ocean and at low /media/ces/2010_005_.pdf

• 14. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  19 CMIP3 GCMs are used (Table 2.1). The horizontal grid spacing of these models varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude. For each 2 Some of the RCM simulations in the ENSEMBLES data base were conducted with funding from other sources, including CES. 5 model, a 198-year time series (1901-2098) obtained /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 15. Awards and press

  our users to the comprehensive web of the Icelandic Road and Coastal Administration, road.is. Appraisal during Bárðarbunga and Holuhraun 2014 - 2015 From Belmont, MA, USA: "Congratulations and thank you for superb coverage and public release of information about the Bárðarbunga eruption 2014 - 2015. I have been on the staff of Harvard SEAS for decades, retired now. I have visited /about-imo/the-web/awards_and_press/

• 16. VI_2020_008

  a precipitation value from a given location based on values from a regular gridded dataset. ................................................................................................. 28 Figure 7. Scatterplots and Q–Q plots comparing daily precipitation from the ICRA dataset and observations with different extraction methods for station Eskifjörður. .................................. 30 /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 17. VI_2013_006

  The lightning current leads to an electromagnetic wave that can be observed over great distances (>10 000 km). The web site of the IMO includes lightning information from the ATDnet system (Arrival Time Difference) of the UK Met Office. This system is based on several out-stations in and around Europe and has been operational since 1988, see Figure 2. One of its stations at Keflavík airport in Iceland /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 18. IPPC-2007-ar4_syr

  Arctic sea ice extent has shrunk by 2.7 [2.1 to 3.3]% per decade, with larger decreases in summer of 7.4 [5.0 to 9.8]% per decade. Mountain glaciers and snow cover on average have declined in both hemispheres. The maximum areal extent of sea- sonally frozen ground has decreased by about 7% in the Northern Hemisphere since 1900, with decreases in spring of up to 15%. Temperatures at the top /media/loftslag/IPPC-2007-ar4_syr.pdf

• 19. VI_2016_006_rs

  and in the uppermost rows of houses below Botnabrún. The most effective mitigation options to improve the landslide hazard situation in southern Seyðisfjörður is draining of the main source areas in Neðri-Botnar in the lower part of the mountainside as well as a construction of a moderately high catching dam above the top row of houses below Botnabrún, and debris retention basins and guiding dams at the lateral /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 20. GA_2009_91A_4_Andreassen

  Fokstugu was used, r was 0.882. The differ- ence in r for the two periods is only 0.015 and doesnot indicate a systematic shift in summer tempera-ture due to the change in station location. Mass balance modelThe mass balance model calculates the mass bal- ance, b(z), as the sum of ablation and solid precip-itation: where Q is energy available for melt, Lm is latentheat of melting and Psolid /media/ces/GA_2009_91A_4_Andreassen.pdf