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Results:

• 31. Keranen_Jaana_CES_2010

  / opportunity identification 4. Risk / opportunity estimation (consequences, probabilities) 1. Scope definition Targets 5. Risk / opportunity evaluation Adaptation, mitigation Risk management Risk analysis Action plan Risk assessment 2. Data collection 2 .2 - … very likely2 .1 – L isääntyvä sadan ta vuositasolla 0-8 % 2. Lisääntyvä sadanta 1 .2 - … 3very likely T urbii nien kapasioteett ia vo idaan /media/ces/Keranen_Jaana_CES_2010.pdf

• 32. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Eyjafjallajo¨kull (E), Tindfjallajo¨kull (Ti), Torfajo¨kull (To) and My´rdalsjo¨kull (M) ice caps. The Gı´gjo¨kull outlet glacier (G) of Eyjafjallajo¨kull is also indicated. The inset map of Iceland shows the location of the study area as well as Langjo¨kull (L), Hofsjo¨kull (H) and Vatnajo¨kull (Va) ice caps and these weather stations: Vı´k (V) in My´rdalur (15 m a.s.l., ca. 30 km south-east /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 33. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  %) 14 (26%) 39 (74%) Gender Number (%) E I S N T F P J Male 100 (48%) 47 (47%) 53 (53%) 15 (15%) 85 (85%) 59 (59%) 41 (41%) 29 (29%) 71 (71%) Female 109 (52%) 66 (61%) 43 (39%) 22 (20%) 87 (80%) 43 (39%) 66 (61%) 21 (19%) 88 (81%) Climatic Change (2012) 112:233–242 237 symposia participants were not significantly different from the preferences of the U.S. general population, which was 49 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 34. 2010_003rs

  Use of relatively located micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir VÍ 2010-003 Skýrsla   f l l l dUse o re ative y ocate micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir, Veðurstofu Íslands VÍ 2010-003 ISSN 1670-8261 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 35. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in ty N at ur e o f u n ce rta in ty Inp ut dat a Mo de l Co ntex t Multi pl e knowl edg e fra m es Ambi guit y Ep istemi c un certaint y (re du cib le) Aleator y u n ce rta in ty (ir red uc ibl e) Pa ramete r val ue s Mode l techni ca l as pe ct s Mo de l st ru ct ur e G re en ho us e ga s em iss io ns X X X X X X X X X X Socio -econo m ic scena rio s X X X X X X X X X XX X X X Fu tu re cl im /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 36. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 37. Case_A___Horsens_Fjord

  increased net precipitation and increased rainfall intensity put pressure on the sewage system and the lake dam. Flooding of the town is expected to occur more frequently. Future flooding storms could be as high as 2,5 meters. The challenges have been divided into two main themes: sea level change and rainfall. NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop /media/loftslag/Case_A___Horsens_Fjord.pdf

• 38. ESC-IASPEI-statement-LAquila-2012-1

  /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 39. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 40. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf