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Results:

• 1. Program

  is the difference between adaptation and adaptive management? 10:20 p3 Trausti Jónsson (IMO, Ice). The UN International Strategy for Disaster Reduction (ISDR) - the WMO method and its application in Iceland 10:50 tea/coffee break 11:15 p4 Tony Rosqvist (VTT, Fin). Group Decision Support Systems - its principles and an application to a flood risk reduction case 11:45 p5 Annika Carlsson-Kanyama (FOI /nonam/workshop/program/

• 2. NONAM_participants

  @geus.dk Jes Pedersen jes.pedersen@ru.rm.dk Jórunn Harðardóttir jorunn@vedur.is Katrín Georgsdóttir kg@arborg.is Laufey B. Hannesdóttir laufeybh@lvp.is Luisa Esteban-Salvador luisaes@unizar.es Matthildur B. Stefánsdóttir matthildur.stefansdottir@vegagerdin.is Nikolai Nawri nikolai@vedur.is Ólafur Pétur Pálsson opp@hi.is Óli Grétar Blöndal Sveinsson olis@lvp.is Philippe Crochet philippe@vedur.is /media/vedurstofan/NONAM_participants.pdf

• 3. Material from the Workshop in Reykjavík 2010

  /nonam/workshop/material/

• 4. Tony_Rosqvist_(VTT,_Fin)

  Tony Rosquist (VTT, Fin) - Group Decision Support Systems - its principles and an application to a flood risk reduction case Tony Rosqvist Adriaan Perrels VTT Technical Research Centre of Finland Finnish Meteorological Institute (FMI) Finland Finland A group decision-making exercise was organized in 2008 as part of an integrated assessment of selected extreme weather events /media/loftslag/Tony_Rosqvist_(VTT,_Fin).pdf

• 5. Alam_Ashraful_CES_2010

  scenario Summer Winter Temp ▲6˚c ▲7˚c. Precip. +10% +30% CO N l d bl2 ear y ou e 11 Forest management principles 1 ) Basal area just before thinning Thinning threshold Energy wood Energy biomass a r e a ( m 2 h a - 1 thinningt i g B a s a l a Basal area just Remaining basal area threshold Dominant height (m) after thinning 12 Management regimes Changes in basal area thinning thresholds /media/ces/Alam_Ashraful_CES_2010.pdf

• 6. Session program Thursday 13. October

  on the long- and on the short-term before large earthquakes Ragnar Stefánsson 10:10 – 10:40 Coffeebreak and poster session 10:40 – 12:10 Oral session - Chair: Peter H. Voss 10:40 – 11:00 High-rate GPS seismology in Iceland Halldór Geirsson et al. 11:00 – 11:20 Rock stress boundaries deduced from rock stress measurements /norsem/norsem2016/program/thursday

• 7. VI_2014_001

  developed for daily and instantaneous index floods. Several models were tested and their parameters estimated by ordinary least square regression after logarithm transformation: bµi(D) = a(Ai) b (7) bµi(D) = a(Ai=Li) b (8) bµi(D) = a(AiPmi) b (9) bµi(D) = a(AiPi) b (10) bµi(D) = a(AiPmi=Zi) b (11) bµi(D) = a(AiPi=Zi) b (12) Where q = (a;b) is the vector of regression parameters, A is the drainage area /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

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

  +2αi )1+αi ) 1−ri + (1 − pi1)(10 + 0.6xi1)1−ri 1 − ri (11) The first mover’s beliefs about the second mover’s type, i.e., the second mover’s β , and her risk aversion both affect the optimal contribution. Depending on the second mover’s choice, the first mover may earn the same as or less than the second mover. Regarding inequity preferences, only the first mover’s disadvantageous inequity aversion /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 9. NONAM_1st_workshop_summary_v3

  work on case studies in break out groups, and plenary discussions. The 11 presentations that were given by scientists and practitioners from all five Nordic countries covered theoretical aspects as well as case studies. Abstracts and slides from the oral presentations are available at http://en.vedur.is/nonam/workshop/. The two break-out groups worked on two different cases: (a) The Horsens /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 10. program17012012

  Airborne Measurements of Volcanic Ash - results from Eyja and the new Met Office Civil Contingency Aircraft Jonathan P. Taylor, UK Met Office 11:15 Observational systems for monitoring of volcanic ash Sibylle von Löwis, Geirfinnur S. Sigurðarson, IMO 11:45 NAME dispersion model, an introduction Jonathan P. Taylor, UK Met Office 12:15 – 13:30 Lunch break The volcanic ash problem /media/vedurstofan/utgafa/hlidarefni/program17012012.pdf