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Results:

• 11. IMO_AnnualReport2014

  ANNUAL REPOR T 2014 2 I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 ?Veðurstofa Íslands 2015 Bústaðavegur 7–9, 108 Reykjavík, Iceland The annual report was drafted by the IMO sta?. Editor: Sigurlaug Gunnlaugsdóttir Design and layout: Hvíta húsið Printing: Oddi ISSN 2251-5607 Cover photo: Gro Birkefeldt Møller Pedersen I N D E X 4 Bárðarbunga 7 Rockslide /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

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

  are organized by self-identified primary research discipline and gender Primary Research Discipline Number (%) E I S N T F P J Biological Sciences 50 (24%) 26 (52%) 24 (48%) 9 (18%) 41 (82%) 22 (44%) 28 (56%) 7 (14%) 43 (86%) Physical Sciences 106 (51%) 56 (53%) 50 (47%) 20 (19%) 86 (81%) 52 (49%) 54 (51%) 29 (27%) 77 (73%) Social Sciences 53 (25%) 31 (58%) 22 (42%) 8 (15%) 45 (85%) 28 (53%) 25 (47 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 13. 2005EO260001

  bursts of seismic tremor (1–3 Hz), and later becoming periodic with energy between 2 and 8 Hz. After 18 October, seismicity increased to three events per day (Figure 2b). Synchronous with this increase, the ISGPS station SKRO (Figure 1b) moved 9 mm westward over the following eight days, and returned to its original position on 1 November (Figure 2c), suggesting subsurface magma movement /media/jar/myndsafn/2005EO260001.pdf

• 14. Paper-Olafur-Rognvaldsson_92

  for Meteorological Research, Reykjavík, Iceland 5Bergen School of Meteorology, Geophysical Insitute, University of Bergen, Norway †Corresponding author: or@belgingur.is, Orkugarður, Grensásvegur 9, 108 Reykjavík ABSTRACT Atmospheric flow over Iceland has been simulated for the period Jan- uary 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the ECMWF. Firstly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 15. Refsgaard_etal-2007-Uncertainty-EMS

  be broader than stated? (7) Further elicit and specify the distribution (shape and percentiles or characterising parameters). (8) Verify with the expert that the distribution that you constructed from the expert’s re- sponses correctly represents the expert’s beliefs. (9) Decide whether or not to aggregate the distributions elicited from dif- ferent experts (this only makes sense if the experts /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 16. ces-glacier-scaling-memo2009-01

  ), the total change in glaciated area may be approximated as DSa = 1 g DVa V1 S1 ; (8) in case DVa < 0 or if DVa > 0 and there is sufficient previously ice-covered space to readvance the ice margin (and DSa = 0 in case DVa >= 0 and there is insufficient space to advance the ice margin). The change in average ice thickness is Dha = V1 +DVa S1 +DSa h1 ; (9) TóJ 8 5.12.2009 Memo in case DVa < 0, and Dha =DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 17. VI_2014_005

  Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri VÍ 2014-005 Skýrsla 2 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland VÍ 2014- 005 ISSN 1670- 8261 Skýrsla +354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Nik olai Nawr i /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 18. VI_2020_005

  00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Guðrún Elín Jóhannsdóttir, Department of Earth Sciences at Uppsala University Abstract Flood risk increases with rising sea levels and coastal settlements need to adapt to this increasing risk. For that, hazard and risk assessments are an important step. Coastal floods have caused prob- lems in Iceland in the past /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

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

  Surface 110, F04001, doi: 10.1029/2005 JF000289. Adalgeirsdo´ttir G., Jo´hannesson T., Bjo¨rnsson H., Pa´lsson F. & Sigurdsson O. 2006. Response of Hofsjo¨kull and southern S. Gudmundsson et al. Mass balance of three ice caps in southern Iceland Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 9 (page number not for citation purpose) Vatnajo¨kull, Iceland, to climate change /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 20. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf