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Results:

• 11. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 12. vanRoosmalen_etal-2009-WRR_2007WR006760

  evapotranspiration decreased by 19% and 22% for the two catchments, showing that the increased biomass of the vegetation only partly compensated for the 30% reduction in transpiration due to stomatal closure, as a result of the higher atmospheric CO2 concentration. [8] The aim of this study is to determine the sensitivity of the hydrological system to a number of meteorological and land use factors, which /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 13. Hydropower, Hydrology

  ) på University of Gloucestershire i Cheltenham 29/9 2009. Roald, L.A. Klimaendringer, flom og skred. Forelesning på kurset: 09/50 Klimatilpasning i samfunnsplanleggingen arrangert av NUSB i Trondheim 10/11-2009. Vehviläinen, B. Climate change and Finlands water resources. Symposium of Large Lakes. March 8, 2010, Lahti, Finland. Veijalainen, N. Climate and Energy Systems (CES): Hydrology /ces/publications/nr/1938

• 14. Observations - Holtavörðuheiði

  Observations - Holtavörðuheiði | Observations | Icelandic Meteorological office Observations - Holtavörðuheiði Mon 1.05 13 GMT -0.3° NNE 7 Max wind : 7 / 10Road temp. : 1.4° 12 GMT -1.8° NNE 7 Max wind : 7 / 10Road temp. : 0.3° 11 GMT -2.3° NNE 7 Max wind : 8 / 10Road temp. : 0.1° 10 GMT -2.8° NNE /m/observations/areas

• 15. Group4

  construction and maintenance. 7. Path dependency, meaning that roads will likely continue to exist even if the underlying need for them decreases. 8. Social shifts, personal ownership of cars no longer seen as necessary. Car-sharing becomes part of a suite of mobility options within the collective transportation system. 9. Behavioral shifts, mobility no longer dominant variable in daily life /media/loftslag/Group4.pdf

• 16. 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

• 17. Horsens_case

  lying areas in the City is illustrated for present climate in Figure 5. It is expected that the future water level of the Horsens fiord will increase by 1 meter by the end of this century. Station 270045: Upstream Lake Nørrestrand 0 0.5 1 1.5 2 2.5 3 3.5 4 1 2 3 4 5 6 7 8 9 10 11 12 Month M ea n d is ch ar g e (m 3 / s) Present: Mean A2: Mean Station 280001: Upstream Bygholm Lake 0 1 2 3 4 5 6 /media/loftslag/Horsens_case.pdf

• 18. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 19. Reykholt-abstracts

  ................................................................................................................... 8 Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9 Lidar measurements of Norwegian glaciers – an overview Neil Arnold* and Gareth Rees .............................................................................................. 10 Calculation of glacier velocity from repeat /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 20. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf