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Results:

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

  ’ on at least 3 of the 4 dichotomies (Myers et al. 1998), and we expect similar patterns among our participants. It should be noted that the MBTI® has a long history of discussion focusing on the reliability and validity of the instrument’s scores (e.g., Carlyn 1977; Carlson 1985; Capraro and Capraro 2002; Salter et al. 2005), and some authors have questioned the utility of the instrument (e.g., Pittenger /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 2. ces-glacier-scaling-memo2009-01

  volume towards a new steady state of the glacier in the case of a “moderate” step change in climate. The relative importance of the mass-balance–elevation feedback and the reduction in ice- covered area may be analysed with reference to the perturbation equation d(DV ) dt = B0+beDA+GeDV = B 0 DV tV ; (3) where the volume time-scale tV is given by tV = 1 ( be=H) Ge ; (4) (Harrison and others, 2001 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 3. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Reykjavı´k IS-101, Iceland 2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France 3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark Keywords Remote sensing; glacier mass balance; regional warming /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

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

  of the model with past observations, it is used to simulate the future response of the glacier during the 21st century. The mass balance model was forced with an ensemble of temperature and precipita- tion scenarios derived from 10 global and 3 regional climate model simulations using the A1B emission scenario. If the average climate of 2000–2009 is maintained into the future, the volume /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. 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

• 6. Daniell_etal-2010

  Christian Huesmann 1, Sophie Rotter 3, Claudia Pahl-Wostl 1, Karina Speil 3, and Wiebke Pohl 1 ABSTRACT. New regulatory water management requirements on an international level increasingly challenge the capacity of regional water managers to adapt. Stakeholder participation can contribute to dealing with these challenges because it facilitates the incorporation of various forms of knowledge /media/loftslag/Daniell_etal-2010.pdf

• 7. 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

• 8. vanRoosmalen_etal-2009-WRR_2007WR006760

  and evapotranspiration to the surface and groundwater system. The vegetation type deter- mines the transpiration properties through the crop factor and the root depth, and the fraction of precipitation that is intercepted by the canopy. Land use changes can therefore reduce or amplify future climate change induced hydrological impacts in a catchment. [3] A number of studies have focused on the effects /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 9. Journal_of_Hydrology_Veijalainen_etal

  an over- all picture (67 sites of varying runoff area sizes) of the changes in floods by 2010–2039 and 2070–2099 using conceptual hydrologi- cal modelling and several climate scenarios and (2) estimating the consequent changes in flood inundation at four selected settle- ments using 2D hydraulic modelling. A further goal is (3) to outline climate change effects regionally as well as in different types /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 10. VI_2014_006

  .......................................................................... 14 2.6 Deterministic predictions ......................................................................... 14 2.7 Forecast evaluation statistics..................................................................... 14 3 Data ........................................................................................................... 14 3.1 Meteorological data /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf