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Results:

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

  images (Fig. 7 and Table 2); with an accuracy of about half the pixel size (Berthier et al., 2005). The magnitude of the SPOT5 velocity in profile DD’ is similar to the observations made in the 1930s (Fig. 6a). A good spatial coverage was obtained by using two SPOT im- ages from late summer 2002, but reliable signals were only obtained for limited areas when an attempt was made to de- termine /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

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

  RM, Capraro MM (2002) Myers-Briggs Type Indicator score reliability across studies: a meta-analytic reliability generalization study. Educ Psychol Meas 62:590–602 Carlson JG (1985) Recent assessments of the Myers-Briggs Type Indicator. J Personal Assess 49:356–365 Carlyn M (1977) An assessment of the Myers-Briggs Type Indicator. J Personal Assess 41:461–473 Clack GB, Allen J, Cooper D et al (2004 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 3. ces-glacier-scaling-memo2009-01

  in Norway was provided by the Norwegian Water Resources and Energy Directorate (NVE). TóJ 12 5.12.2009 Memo References Bahr, D. B., M. F. Meier and S. D. Peckham. 1997. The physical basis of glacier volume–area scaling. J. Geophys. Res., 102(B9), 20,355–20,362. Björnsson, H., and F. Pálsson. 2008. Icelandic glaciers. Jökull, 58, 365–386. Fenger, J. (Ed.). 2007. Impacts of Climate Change on Renewable /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 4. VI_2015_009

  estimates are required at locations where streamflow series are very short or where no data are available, making a direct estimation im- possible. Regional flood frequency analysis such as the index flood method (IFM) (Dalrymple, 1960) offers a solution to this problem. The idea is to trade space for time and compensate for the lack of information at the site of interest by using flood data from other /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 5. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

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

  Icelandic glaciers. Jo¨kull 58, 365
  386. Bjo¨rnsson H., Pa´lsson F. & Haraldsson H.H. 2002. Mass balance of Vatnajo¨kull (1991
  2001) and Langjo¨kull (1996
  2001), Iceland. Jo¨kull 51, 75
  78. Bouillon A., Bernard M., Gigord P., Orsoni A., Rudowski V. & Baudoin A. 2006. SPOT 5 HRS geometry performance: using block adjustments as a key issue to improve quality of DEM generation. ISPRS Journal /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 7. 2010_005_

  /media/ces/2010_005_.pdf

• 8. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf