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Results:

• 11. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 12. 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

• 13. 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

• 14. 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

• 15. 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

• 16. 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

• 17. 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

• 18. 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

• 19. 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

• 20. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf