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Results:

• 1. 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

• 2. 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

• 3. 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

• 4. 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

• 5. ces-glacier-scaling-memo2009-01

  ), the total change in glaciated area may be approximated as DSa = 1 g DVa V1 S1 ; (8) in case DVa < 0 or if DVa > 0 and there is sufficient previously ice-covered space to readvance the ice margin (and DSa = 0 in case DVa >= 0 and there is insufficient space to advance the ice margin). The change in average ice thickness is Dha = V1 +DVa S1 +DSa h1 ; (9) TóJ 8 5.12.2009 Memo in case DVa < 0, and Dha =DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 6. 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

• 7. Journal_of_Hydrology_Veijalainen_etal

  of the study sites, which correspond to the discharge observation stations. Study sites (a–e) selected for further evaluation are described in Table 1. Circles are unregulated and squares regulated sites. N. Veijalainen et al. / Journal of Hydrology 391 (2010) 333–350 335 Author's personal copy (Table 2); in the winter they are almost twice as high as in summer. Precipitation changes are between 8 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 8. VI_2009_006_tt

  during the Holocene . . . . . . . . . . . . . . 6 2.5 Jökulhlaups in America and Asia at the end of the last glaciation . . . 7 2.6 Jökulhlaup sediment concentration and Lahars . . . . . . . . . . . . . 8 3 The Skaftá cauldrons and jökulhlaups in Skaftá 9 3.1 The subglacial lakes . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 3.2 Jökulhlaups in Skaftá /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 9. 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

• 10. Daniell_etal-2010

  to provide input to WFD implementation [6; 5; 7; 3] [8; 4]. This previously highly political issue became business as usual for stakeholders and authorities alike, and the process outcomes were a welcome input into the formal participatory process of the Bezirksregierung [2; 1]. Collaborative process design in a Trialogue team The second challenge relates to the design of a participatory process /media/loftslag/Daniell_etal-2010.pdf