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Results:

• 41. CES_D2.4_task1

  MIETOINEN SAARI FI +60:37:48 +21:52:12 13 T 706 TURKU AIRPORT FI +60:30:00 +22:16:12 47 TP 708 JOKIOINEN OBSERVATOR FI +60:49:12 +23:30:00 104 T 710 UTTI AIRPORT/VALKEAL FI +60:54:00 +26:55:48 99 T 717 KAUHAVA AIRPORT FI +63:06:00 +23:01:48 42 T 718 AHTARI MYLLYMAKI FI +62:31:48 +24:13:12 157 /media/ces/CES_D2.4_task1.pdf

• 42. GA_2009_91A_4_Andreassen

  with precipitation data from Fokstua asinput and a much lower correlation (r2=0.48) wasobtained (De Woul and Hock 2005; Table 2) thanthe r2 of 0.75 we obtained by using a combinationof Bulken and Røldal. Their observation period was shorter (45 years) than the period used in thisstudy (58 years). Rasmussen and Conway (2005)obtained r2=0.63 using an upper-air model for theperiod 1948/49–1998/99 /media/ces/GA_2009_91A_4_Andreassen.pdf

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

  aversion should influence the first mover’s decision. The 98 Public Choice (2012) 151:91–119 Fi g. 1 O pt im al co n tr ib u tio n de pe nd in g o n α , r an d p Public Choice (2012) 151:91–119 99 Table 1 The predicted effect of intrinsic preferences on first and second movers’ contributions 1st mover 2nd mover Disadvantageous Negative None inequity aversion Advantageous None Positive inequity /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 44. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 45. IPPC-2007-ar4_syr

  judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 46. Bárðarbunga 2014 - September events

  September 2014 10:00 - earthquakes since 16 August 2014 Earthquakes during the first month of events (from 16.09.2014 at 00:00 until 15.09.2014 at 22:20): all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 25.000 - - - - - - - checked ~ 5.900 ~ 4.100 ~ 760 ~ 120 ~ 250 ~ 680 ~ 70 ~10 M3.0-3.9 186 99 74 6 /earthquakes-and-volcanism/articles/nr/3001

• 47. Bardarbunga-2014_September-events

  - - - - - - - checked ~ 5.900 ~ 4.100 ~ 760 ~ 120 ~ 250 ~ 680 ~ 70 ~10 M3.0-3.9 186 99 74 6 2 3 1 1 M4.0-4.9 43 7 34 1 1 0 0 0 M>5.0 23 0 23 0 0 0 0 0  HB/HBT: Herðubreið and Herðubreiðartögl  TFJ: Tungnafellsjökull  Kverkfj.: Kverkfjöll  Kistufell: Cluster north of Bárðarbunga that was active during the first days  automatic: Automatically detected /media/jar/Bardarbunga-2014_September-events.pdf

• 48. VI_Arsskyrsla_2018_vef

  /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 49. Bárðarbunga 2014 - September events

  September 2014 10:00 - earthquakes since 16 August 2014 Earthquakes during the first month of events (from 16.09.2014 at 00:00 until 15.09.2014 at 22:20): all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 25.000 - - - - - - - checked ~ 5.900 ~ 4.100 ~ 760 ~ 120 ~ 250 ~ 680 ~ 70 ~10 M3.0-3.9 186 99 74 6 /earthquakes-and-volcanism/articles/nr/3001/

• 50. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941