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Results:

• 1. 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

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

  of the glaciers. An up to 8 m thick winter snow layer was measured in the accumulation area (∼4 m w.e.). Ice melt of up 10 m w.e. was measured in the lowest part of the ab- lation zone in summer, and 2 m w.e. was melted during win- ter. Taking into account ∼2 m of annual rainfall, the runoff from this part of the glacier was estimated as ∼14 m w.e. per year; a surprisingly high value (Ahlmann, 1939 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 3. 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

• 4. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 5. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 6. VI_2015_006

  6 Net downward shortwave radiation flux at the surface .................................... 18 7 Net downward longwave radiation flux at the surface ..................................... 19 8 Net downward total radiation flux at the surface............................................ 20 9 Upward sensible heat flux from the ground .................................................. 22 10 Air /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 7. 2010_005_

  decade within the 2004–50 period, for the UKMO HadCM3, and the MPI ECHAM5-r3. . . . . . . . . . . . . 28 7 Mean annual surface air temperature and total precipitation during the 1961–90 control period, and linear trends within the 1958–2001 period, for the ERA-40 reanalyses. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 8 Differences between the RCM and underlying /media/ces/2010_005_.pdf

• 8. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  are organized by self-identified primary research discipline and gender Primary Research Discipline Number (%) E I S N T F P J Biological Sciences 50 (24%) 26 (52%) 24 (48%) 9 (18%) 41 (82%) 22 (44%) 28 (56%) 7 (14%) 43 (86%) Physical Sciences 106 (51%) 56 (53%) 50 (47%) 20 (19%) 86 (81%) 52 (49%) 54 (51%) 29 (27%) 77 (73%) Social Sciences 53 (25%) 31 (58%) 22 (42%) 8 (15%) 45 (85%) 28 (53%) 25 (47 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 9. 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

• 10. VI_2015_009

  ..................................................................................... 7 2.3 Meteorological data ................................................................................ 8 2.4 Other data ............................................................................................ 8 3 Index flood method ...................................................................................... 11 3.1 General /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf