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  • 11. 47th Nordic Seismology Seminar

    buy a "Flybus Plus" ticket, further transportation from BSÍ terminal in central Reykjavík to the hotel is included. Get a return ticket for smooth transportation back to the airport, the same way you came. You do not need to book your ticket in advance. The Flybus operates for all arriving flights, and even in case of flight delays it will wait for the passengers.To get around in ReykjavíkCity /norsem/norsem2016/transportation/
  • 12. VI_2015_009

    ) Mean absolute error (MAEµ) Nash-Sutcliffe efficiency (NSµ) (Nash & Sutcliffe, 1970) With RMSEµ(%) = s 1 N N i=1 bµi(D) µi(D) µi(D) 2 x100 (4) MAEµ(m 3=s) = 1 N N i=1 jbµi(D) µi(D)j (5) NSµ = 1 Ni=1 bµi(D) µi(D) 2 Ni=1 µi(D) E[µi(D)] 2 (6) 12 where µi(D) is the reference index flood at target site i defined by the arithmetic mean of ob- served AMF, and N the total number /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 13. esa_flyer_new

    Work Group: Energy System Analysis http://www.os.is/ces Energy System Analysis is a Work Group within the Nordic research project Climate and Energy Systems (2007-2010). This project is in many ways a follow up on the CE-project (2003-2006), where energy system analyses were carried out for the expected energy system in 2010 using future climate (2070-2100). That study illustrated future climate /media/ces/esa_flyer_new.pdf
  • 14. IMO_AnnualReport2014

    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 Monitoring Bárðarbunga Rifting events, as in Bárðarbunga 2014-2015, are rather rare and can be part of a rifting episode that lasts months, years or even decades. One example of a rifting episode on land is Iceland’s Krafla fires in 1975-1984. Whether the Bárðarbunga event is the beginning of a prolonged episode /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 15. ces-glacier-scaling-memo2009-01

    ) is considered as a sequence of steps corresponding to n individual glaciers of different sizes (with volumes vi and areas si for i = 1 to n), or using V (v) = Z v 0 1 g dS ds dx ; (7) where the slope of the area distribution function, dS=ds, is considered as a function of ice vol- TóJ 5 5.12.2009 Memo 0 50 100 150 200 0 5 10 15 20 25 Cumulative area (km2) Area (km 2 ) 0 5 10 15 0. 0 0. 5 1. 0 1. 5 2. 0 2. 5 /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 16. Alam_Ashraful_CES_2010

    FOREST BIOMASS FOR ENERGY PRODUCTION – POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki School of Forest Sciences, University of Eastern Finland, Joensuu F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on Oslo, Norway 2 June, 2010 Contents • Forestry in Finland • Challenges • Objectives /media/ces/Alam_Ashraful_CES_2010.pdf
  • 17. Kjellstrom_Erik_CES_2010

    ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf
  • 18. Tornado_Impacts_-_FMI_Presentation

    % 40.00% 50.00% 0.00% 10.00% 20.00% 0 1 2 3 4 5 F-Scale Category Casualties and F-scale Injuries by F-Scale 30.00% 40.00% 0.00% 10.00% 20.00% 0 1 2 3 4 5 F-Scale Category Why Study Tornadoes • How do tornadoes kill people, and how can we reduce casualties? • Do warnings reduce casualties? • Do people suffer from low probability event bias? • How do manufactured homes and tornado shelters affect /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
  • 19. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

    to receivers when they are obliged to be matched with a receiver, compared to the situation where they can decide to be alone or to be matched with a receiver. Public Choice (2012) 151:91–119 103 which the responder accepted the sender’s distribution, so that s i − 1 is the decision number minus one of the last decision in which the responder rejected the distribution of the sender. This individual /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
  • 20. Kok_JGEC658_2009

    three concepts C1, C2, and C3 with: state vectorA ¼ ð1;0;1Þ adjacency matrix E ¼ 1 1 0 0:1 0 0 0 0:5 1 0@ 1A newstate vectorB ¼ A E ¼ ð1;0;1Þ  1 1 0 0:1 0 0 0 0:5 1 0@ 1A ¼ 1 ð1;1;0Þ þ 0 ð0:1;0;0Þ þ 1 ð0;0;5;1Þ ¼ ð1;1;0Þ þ ð0;0;0Þ þ ð0;0;5;1Þ ¼ ð1;1:5;1Þ The calculation of a new state vector can be repeated infinitely, during which four possible patterns can emerge: (1) the concepts can /media/loftslag/Kok_JGEC658_2009.pdf

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