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Results:

• 21. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 22. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 23. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 24. VI_2019_009

  of the 1st cloud layer. ................. 14 3 Height of the 1st cloud layer. Automatic records as a function of manual obser- vations. ................................................................................................ 15 4 Number of records as a function of cloud amount of the first layer. ................... 16 5 Cloud amount of the 1st layer. Automatic records as a function of manual /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 25. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 26. VI_2015_005

  ..................................................................... 14 5 Spatial distribution of cyclone centres ............................................................. 16 6 Upper-level flow associated with different MSLP modes .................................... 23 7 Weather anomalies associated with different MSLP modes ................................ 26 8 Summary /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 27. Reykholt-abstracts

  ....................................................................................... 16 Mass balance and volume changes of Eyjafjallajökull ice cap, from 1984 to 2010, deduced by multi-temporal elevation maps Victoria H. Hamilton Morris ................................................................................................. 17 Construction and analysis of lidar mosaics of sea ice floe /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 28. Observations - Skarðsheiði Miðfitjahóll

  -3.4° NE 10 Max wind : 11 / 13 09 GMT -4.3° NE 10 Max wind : 11 / 14 08 GMT -4.8° NE 11 Max wind : 11 / 13 07 GMT -5.3° NE 9 Max wind : 10 / 13 06 GMT -5.3° NE 10 Max wind : 10 / 14 05 GMT -5.3° NE 10 Max wind : 12 / 16 04 GMT -5.2° NE 11 Max wind : 12 / 14 03 GMT -5.1° NE 12 Max wind : 13 / 16 02 GMT -4.9° NE 13 Max wind /m/observations/areas

• 29. 2005

  2005 Ísflug 16. mars 2005 © Garðar Þór Magnússon Hafís norðan og vestan við landið 16. mars 2005. Myndin er tekin í /sea-ice/sea/gallery/2005/bigimg/2653

• 30. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf