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Results:

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

  Personality type differences between Ph.D. climate researchers and the general public: implications for effective communication C. Susan Weiler & Jason K. Keller & Christina Olex Received: 27 August 2009 /Accepted: 28 July 2011 / Published online: 2 September 2011 # The Author(s) 2011. This article is published with open access at Springerlink.com Abstract Effectively communicating the complexity /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 2. 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

• 3. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 4. VI_2015_009

  J600v berg 2.utg) were also used in this study. Table 1. Main characteristics of river basins used in this study. River Name Type Area Mean Percentage Mean annual Period / (km2) elevation glacier precipitation for Gauging (m a.s.l) (mm) streamflow station (1961-2014) data vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014 vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014 vhm66 Hvítá (Borgarfirði) L+J 1577 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

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

  /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 6. 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

• 7. 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

• 8. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 9. vanRoosmalen_etal-2009-WRR_2007WR006760

  for the period 1971–2004 of which 1971–1989 is a spin-up period, where the model is allowed to adjust itself to the prevailing hydrological conditions, while the period 1990– 2004 is used as the period for the hydrological interpretations. 3.3.1. Unsaturated Zone [28] Unsaturated zone processes are computed by a two- layer water balance method [Yan and Smith, 1994] available in the MIKE SHE system [DHI /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 10. VI_2014_006

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