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Results:

• 1. 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

• 2. 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

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

  surface velocity (Table 2 and com- parison on profile DD’ in Fig. 6a), indicating that the model captures the large-scale flow pattern of the glacier. The 20th century glacier runoff anomalies, relative to a ref- erence runoff computed at the start of the model simulations, from the area that was ice-covered at LIAmax (234 km2) was computed from the mass balance and precipitation fields /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. ces-glacier-scaling-memo2009-01

  is ice flux and b is mass balance. For (small) changes in glacier geometry with respect to a datum (often steady) state, perturbations in ice thickness, flux and mass balance will satisfy ¶(Dh) ¶t + ¶(Dq) ¶x = Db or ¶(Dh) ¶t +~ (D~q) = Db : (2) Changes in mass balance are the driving factor of glacier changes in climate change simu- lations. If the datum glacier is initially comparatively close /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 6. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /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. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  RESEARCH/REVIEW ARTICLE Response of Eyjafjallajo¨kull, Torfajo¨kull and Tindfjallajo¨kull ice caps in Iceland to regional warming, deduced by remote sensing Sverrir Gudmundsson,1 Helgi Bjo¨rnsson,1 Eyjo´lfur Magnu´sson,1 Etienne Berthier,2 Finnur Pa´lsson,1 Magnu´s Tumi Gudmundsson,1 Tho´rdı´s Ho¨gnado´ttir1 & Jørgen Dall3 1 Institute of Earth Sciences, University of Iceland, Sturlugata 7, Askja /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.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

  Reykjavík Philippe Crochet, Icelandic Met Office   Contents 1 Introduction ................................................................................................ 7 2 Methods ..................................................................................................... 9 2.1 WaSiM-ETH......................................................................................... 9 2.2 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf