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• 41. Safetravel

  measure of leaving a travel plan behind. Travel Plan One of the most important things to do when preparing a journey is to make a detailed travel plan and leave with someone who can act if needed. Travel plan should always include the following information: Date of travel, departure time and arrival time Name of those who travel, phone number or other telecommunication Accommodation (GPS /about-imo/news/nr/2707

• 42. Program

  on the afternoon of Friday, 27 August 2010 (at a time that enables catching late return flights to Norway and Denmark). Day one: 26 August 2010 9:00 opening and welcome by local representative Sigrún Karlsdóttir and by Adriaan Perrels (FMI, Fi) as NONAM coordinator 9:20 p1 Jens Christian Refsgaard (GEUS, Dk). Uncertainty and Risk - terminology and concepts 9:50 p2 Gareth James Lloyd (DHI, Dk). What /nonam/workshop/program/

• 43. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 44. ces-oslo2010_proceedings

  Floods in Norway under a near future 2021-2050 climate: Hydrological projections for rainfall vs. snowmelt floods and their uncertainties ................................................................................................................................ 32 Veijalainen, N. and Vehviläinen, B. Climate change and lake regulation in Finland – Impacts and adaptation possibilities /media/ces/ces-oslo2010_proceedings.pdf

• 45. ces-glacier-scaling-memo2009-01

  of melt water from glaciated areas in long integrations for a warming climate. Glacier dynamics This problem can be qualitatively analysed by considering the continuity equation for ice vol- ume, which may be expressed as ¶h ¶t + ¶q ¶x = b or ¶h ¶t +~ ~q = b ; (1) for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions, respectively. h is ice thickness, q or ~q /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 46. Kok_JGEC658_2009

  Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.pdf

• 47. Weather stations

  data ÁsbyrgiNorth EsjObs.ForecastMeteogramInfo.Obs. data ÁsgarðurBreiðafjsjForecastMeteogramInfo.Obs. data ÁsgarðurBreiðafjskObs.Info.Obs. data Return to the top of the page B BakkagerðiE coastalsjObs.Info.Obs. data Básar á GoðalandiSouthsjObs.Info.Obs. data BiskupshálsNorth EsjObs.Info.Obs. data BíldudalurWest fjsjObs.ForecastMeteogramInfo.Obs. data /weather/stations/

• 48. 2010_005_

  periods of time and over smaller spatial scales. In general, regional climate projections are derived either directly from one or more general cir- culation model (GCM) runs, or through additional numerical or statistical downscaling of these large-scale fields. Numerical downscaling uses higher-resolution regional climate models (RCMs) over a limited area to refine global GCM simulations. Problems /media/ces/2010_005_.pdf

• 49. Moellenkampetal_etal-2010

  Coad 5, Jean-Emmanuel Rougier 6, Matthew Hare 7, Natalie A. Jones 8, Albena Popova 4, Dominique Rollin 3, Pascal Perez 9,10, and Stewart Burn 11 ABSTRACT. Broad-scale, multi-governance level, participatory water management processes intended to aid collective decision making and learning are rarely initiated, designed, implemented, and managed by one person. These processes mostly emerge from /media/loftslag/Moellenkampetal_etal-2010.pdf

• 50. CES_D2.4_solar_CMIP3

  global radiation), i.e., the sum of the direct and diffuse solar radiation. The quantity can be expressed in W/m2 or MJ/m2 per time unit. In this account, changes in incident radiation are viewed both in absolute1 and percentage terms. Model output data were downloaded from the CMIP3 data archive. There were a few models for which the simulation for one of the three scenarios was missing; in those /media/ces/CES_D2.4_solar_CMIP3.pdf