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Results:

• 41. BIVM_windrose_2005-2014

  N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 114 8 128 7 84 9 36 1 26 0 13 9 24 3 65 4 136 4 250 3 366 4 298 8 189 6 146 9 99 9 160 6 111 5 83 5 86 1 86 4 80 0 82 6 92 4 96 3 97 5 124 9 109 5 127 7 122 4 115 3 88 0 61 9 52 3 55 3 96 0 109 9 Wind rose BIVM January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 /media/vedur/BIVM_windrose_2005-2014.pdf

• 42. Kok_JGEC658_2009

  and that paving major roads will lead to deforestation. C3: Conservation units. A large percentage of the Amazon (close to 33%) is classified as some kind of protected area. This includes indigenous reserves, federal parks and national parks. Only about 5% is strictly protected, although it is argued that ‘paper parks’ can also be effective. C4: Forest accessibility. The amount of forest /media/loftslag/Kok_JGEC658_2009.pdf

• 43. EEA

  national challenges, such as drought, floods or storm surges Adaptation policies and practices in cities, agriculture and in coastal areas The need to think beyond national borders Participants are those countries and actors involved in the EEA Grants programmes and/or in the development of adaptation policies in the EU. Árni Snorrason, Dir. General of the Icelandic Meteorological Office /about-imo/news/nr/2763

• 44. Snorrason_Arni_CES_2010

  Bodies NordForsk Nordic Innovation Centre Nordic Energy Research Programme timeframe: 2009-2013 Calls for proposals will begin in 2009 Toppforskningsinitiativet (TFI) • Aims of the TFI Programme • Profile the Nordic region as a leader within certain areas of the energy and climate sectors • Strengthen national research and innovation systems • Create larger professional communities which extend /media/ces/Snorrason_Arni_CES_2010.pdf

• 45. Factsheet_Bardarbunga_20141027

  is increasing in Bardarbunga. A cauldron in the southeast corner of Bardarbunga has deepened about 25 meters over a one month period. The depression is considered to be linked to the depression of the Bardarbunga caldera.  Over 70 smaller earthquakes are detected in the dyke over the weekend. The biggest was M2.1 at 11:51 on Sunday.  GPS measurements in the active area show minor changes /media/jar/Factsheet_Bardarbunga_20141027.pdf

• 46. Factsheet_Bardarbunga_20141031

  around magnitude M1,0 and smaller.  GPS measurements in the active area show minor changes. A recommendation by the Scientific Advisory Board of the Icelandic Civil Protection: The Scientific Advisory Board concludes that it is necessary to increase monitoring of SO4 so it is possible to evaluate the concentration of sulphuric acid particles and its potential influence on health. Air /media/jar/Factsheet_Bardarbunga_20141031.pdf

• 47. 2011_005

  transfer and preparation. 3. Assessment of IP-based communication options for dial-up connections. 4. Review of station locations and possibilities for network optimization. 5. Appraisal of data processing, including existing drawbacks, alternative software, future needs for monitoring purposes, data archival, and sharing of CGPS data. 8 1.3 Modifications to original aims As work progressed /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 48. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  individuals act like homo-œconomicus agents (see for example Andreoni 1988; Berg et al. 1995; Camerer 2003; Forsythe et al. 1994; Isaac et al. 1984). Recent developments in public-choice theory have taken a behavioral approach to broaden the analysis of collective action. The introduction of social preferences, such as altruism, inequity aversion or trust, may mean that optimal collective choices /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 49. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 50. raisanen_ruosteenoja_CES_D2.2

  Model Institution BCCR-BCM2.0 Bjerknes Centre for Climate Research, Norway CGCM3.1 (T47) Canadian Centre for Climate Modelling and Analysis CGCM3.1 (T63) same as previous CNRM-CM3 Météo-France CSIRO-MK3.0 CSIRO Atmospheric Research, Australia ECHAM5/MPI-OM Max Planck Institute (MPI) for Meteorology, Germany ECHO-G University of Bonn and Model & Data Group, Germany; Korean Meteorological Agency GFDL /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf