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Results:

• 41. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 42. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 43. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  1 PhD Workshop preceding Adaptation Research Conference – 27 & 28 August, Helsinki Climate change adaptation - Analysis, Planning and Implementation Programme Venue: Rantapuisto, Ramsinniementie 14, FIN-00980 HELSINKI directions for travel can be found at the conference web site http://www.nordicadaptation2012.net/ Informal start at 26 August On Sunday evening 8pm an informal get /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 44. Group-1_Scenarios-for-AWM

  i on c a p ac i t y A r ea of r e s i d en c e (Flood p r one /non p r one a r eas) Un c e r t a n t i e s H i g h wi l l i n g n e s s t o p a y L o w wi l l i n g nes to pay D i k e s H i gh t a x a t i on - E arly w arn i n g s y s t e m s - Sof t s t r uct u r a l m e as u r e s -Community training L o w taxation Risk P e r c e p t i o n B e n e f i /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 45. 2010_017

  of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf

• 46. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 47. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf

• 48. raisanen_ruosteenoja_CES_D2.2

  /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 49. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 50. Statistical Analysis

  & Kjellstrom, E. Analysis of possible changes in intense and extreme wind speeds over northern Europe under climate change scenarios. Climate Dynamics, DOI 10.1007/s00382-010-0955-3 (In press). Reihan, A. Koltsova, T., Kriauciuniene, J., Lizuma, L. & Meilutytë-Barauskienë, D. (2008). Changes in river runoff in Baltic States in 20th century and its relation to climate change. Nordic Hydrology 33 /ces/publications/nr/1943