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• 31. The weather in Iceland in 2018

  0,0 Blönduós 3,8 # 9 15 -0,1 Grímsey 4,1 1,8 5 145 0,2 Akureyri 4,6 1,3 14 138 0,2 Grímsstaðir 2,1 1,7 9 112 0,4 Miðfjarðarnes 4,0 # 4 19 0,6 Skjaldþingsstaðir 4,6 # 4 24 0,6 Egilsstaðir 4,6 1,7 5 64 0,6 Dalatangi 5,2 /about-imo/news/the-weather-in-iceland-in-2018

• 32. Factsheet_Bardarbunga_20150130

  of seismicity with respect to longitudes. NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT Graph a Graph b Figure 7 Graph a) shows a time series for the GPS station in Vonarskad (VONC), the station is labelled with a black box on the earthquake map above. The time series shows a change in the location of the station to the north (top /media/jar/Factsheet_Bardarbunga_20150130.pdf

• 33. Group2-report

   to changing climate conditions. This includes changes in  production modes and infrastructure. In the third set of socio economic conditions the society is willing to  change their lifestyle, which allows the implementation of adaptive measurements which can be  considered as out of the box solutions, e.g. abandoning agriculture completely. In general in all three socio  economic condition sets /media/loftslag/Group2-report.pdf

• 34. Refsgaard_2-uncertainty

  - nitrate reduction in underground medium medium large large large Model technical uncertainty - numerical approximation small small medium small - bugs in software medium medium small SUM: Importance Type of uncertainty Error propagation Box 1 Error propagation rules using standard deviation (σ ) Addition and Subtraction: z = x + y + .. or z = x - y - .. ..)()( 22 ++= yxz σσσ /media/loftslag/Refsgaard_2-uncertainty.pdf

• 35. BIBD_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 36 2 69 4 138 2 187 3 151 2 106 7 83 1 58 1 36 0 20 3 17 6 14 5 14 9 11 0 10 6 13 0 16 7 29 8 55 2 73 0 95 6 140 7 98 9 41 9 20 2 17 7 8 1 6 4 4 8 3 7 5 7 4 4 4 5 7 3 9 2 18 5 Wind rose BIBD January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIBD_windrose_2005-2014.pdf

• 36. Paper-Olafur-Rognvaldsson_91

  : Regional climate modeling revisited. J. Geophys. Res., 104(D6), 6335–6352. Grell, G. A., Dudhia J. and Stauffer D. R. 1995. A description of the fifth- generation Penn State/NCAR Mesoscale Model (MM5). NCAR Tech. Note NCAR/TN-398+STR, 138 pp. Jóhannesson, T., Aðalgeirsdóttir G., Ahlstrøm A., Andreassen L. M., Björnsson H.,de Woul M., Elvehøy H., Flowers G. E., Guðmundsson S., Hock R., Holm- lund P /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 37. Paper-Olafur-Rognvaldsson_92

  and hydrologic models at regional scale. Mon. Wea. Rev., 128(6), 1681–1706. Grell, G. A., Dudhia J. and Stauffer D. R. 1995. A description of the fifth- generation Penn State/NCAR Mesoscale Model (MM5). NCAR Tech. Note NCAR/TN-398+STR, 138 pp. Jasper, K., Gurtz J. and Lang H. 2002. Advanced flood forecasting in Alpine watersheds by coupling meteorological observations and forecasts with a dis- tributed /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 38. raisanen_ruosteenoja_CES_D2.2

  1 Probabilistic forecasts of temperature and precipitation change based on global climate model simulations (CES deliverable 2.2) Jouni Räisänen1 Kimmo Ruosteenoja2 19 December 2008 1 Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland Email: jouni.raisanen@helsinki.fi 2 Finnish Meteorological Institute, P.O. Box 503, FI-00101 Helsinki, Finland Email /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 39. IPPC-2007-ar4_syr

  period in the last 500 years and likely the highest in at least the past 1300 years. {WGI 6.6, SPM} 2 Likelihood and confidence statements in italics represent calibrated expressions of uncertainty and confidence. See Box ‘Treatment of uncertainty’ in the Introduction for an explanation of these terms. 3 Excluding tsunamis, which are not due to climate change. Extreme high sea level depends /media/loftslag/IPPC-2007-ar4_syr.pdf

• 40. Climate Report

  /longitude box extending from 10–30W and 60–70N) revealed that the model ensemble average exhibited considerable warming in the last decades of the 20th century and into the 21st, but the warming rate was half of the warming rate that actually occurred. If the CMIP5 ensemble average warming is used as an indicator of the forced (anthropogenic) warming trend, then about half of the recent observed /climatology/iceland/climate-report