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Results:

• 21. 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

• 22. 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

• 23. 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

• 24. 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

• 25. VI_2015_005

  Office Contents 1 Introduction ................................................................................................ 7 2 Data ........................................................................................................... 8 3 Atmospheric variability connected to pressure changes ..................................... 11 4 Identification of cyclone centres /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 26. Lorenzoni_Pidgeon_2006

  PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN AND USA PERSPECTIVES IRENE LORENZONI and NICK F. PIDGEON∗ Centre for Environmental Risk and Tyndall Centre for Climate Change Research, Zuckerman Institute for Connective Environmental Research, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK E-mail: i.lorenzoni@uea.ac.uk Abstract. If uncontrolled, human influences /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 27. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51 A.6 Höfn . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 53 A.7 Landeyjar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 55 A.8 Langanes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 57 A.9 Meðallandssveit /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 28. VI_2016_006_rs

  of W-Strandartindur and the gullies below .................................................................................................. 23 4.5 Areas 7 and 8: Botnabrún ........................................................................ 24 4.6 Areas 9 and 10: Nautaklauf and Klauf ........................................................ 24 5 Assessment of the hazard potential /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 29. VI_2019_009

  obser- vations. ................................................................................................ 16 6 Number of records as a function of the total cloud cover. ................................ 17 7 Total cloud cover. Automatic records as a function of manual observations. ........ 17 8 Records from the manual station. When every record over 20 km has been mapped to the range /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 30. VI_2020_004

  5 Contents Figures ........................................................................................................................................ 6 Tables .......................................................................................................................................... 8 Abstract /media/vedurstofan-utgafa-2020/VI_2020_004.pdf