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Results:

• 1. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

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

  information. The MBTI®, and similar assessments, utilize a series of questions to assign an individual’s inherent preferred type for each of four dichotomies, resulting in 16 possible personality types (Myers et al. 1998). While we all use each of the dichotomous categories to some extent, they are considered as innate psychological preferences, akin to preferences for left- or right-handedness /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 3. 2010_005_

  Björnsson, Icelandic Meteorological Office   Contents 1 Introduction 9 2 Data and Methodology 11 3 Spatial Variability of Climate Trends 13 3.1 Surface Air Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 4 Long-Term Trends of Annual Mean Values 16 4.1 Surface Air /media/ces/2010_005_.pdf

• 4. VI_2015_009

  ....................................................................................................... 13 4.1 Delineation of homogeneous regions .......................................................... 13 4.2 Regional growth curves ........................................................................... 15 4.2.1 Index flood modelling................................................................... 16 4.2.2 Flood quantile estimation /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 5. ces-glacier-scaling-memo2009-01

  with the following equations a0i = ai Dgi ; g 0 i = gi +Dgi ; (14) and z0i = ai zi Dgi (yi h1) ai Dgi ; y0i = yi +Dha ; if Dgi < 0 (15) or z0i = zi ; y 0 i = gi (yi +Dha)+Dgi (zi +h1 +Dha) gi +Dgi ; if Dgi > 0 ; (16) where the primed quantities denote the updated end-of-hydrological-year values of the corre- sponding quantities at the beginning of the hydrological year. The average elevation of the TóJ 10 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 6. vanRoosmalen_etal-2009-WRR_2007WR006760

  /a in dry summers, which is the maximum amount licensed by the local government. 80% of the water is abstracted from aquifers located above
  20 masl [Henriksen and Sonnenborg, 2003]. 3. Methods 3.1. Climate-Forcing Data [16] The confidence in Atmosphere-Ocean general circu- lation models (GCM) providing credible quantitative esti- mates of future climate change has increased the past few years /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 7. 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

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

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 9. 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

• 10. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf