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Results:

• 31. Tony_Rosqvist_(VTT,_Fin)

  alternatives where calculated and shown as bar graphs for value comparison. Also a sensitivity analysis is possible, thereby showing the robustness of the results. The presentation reviews briefly the approach used in the TOLERATE project. In particular the required information from the participants, the main modeling assumptions and the graphical results of the case study are highlighted /media/loftslag/Tony_Rosqvist_(VTT,_Fin).pdf

• 32. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  ). The surface area of the fiord is approximately 46 km2 and the mean depth is 2.9 m besides a narrow shipping channel with a depth between 7 and 22 m. The catchment area is 517 km2 and dominated by agriculture (75%) with small areas of forests, wetlands, lakes and urban areas. The annual freshwater input is in the order of 100 Mm3, where approximately 70% is channelled through two main creaks /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 33. Case_A___Horsens_Fjord

  already exist today. What is crucial is the ability to combine individual solutions from different sectors and think about the positive aspects of climate changes. A good combination can actually create new values for society and make the coming work considerably less expensive. The key concept is good processes between different players involved in climate change adaptation. With an open /media/loftslag/Case_A___Horsens_Fjord.pdf

• 34. Crochet_Philippe_CES_2010

  and 25% coldest years All years 1971-2000 25% coldest 25% warmest Change in number of flood events (POT) between 25% warmest and 25% coldest years POT > median Q peaks (71-00) barb2right +22% +1.7°CCatchment name POT > mean annual maximum Q (71-00) SW rain-shadow barb2right +156% barb2right -56% North rain-shadow South-SW exposedCenter North Catchment name Summary • All catchments showed signs /media/ces/Crochet_Philippe_CES_2010.pdf

• 35. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 36. Wind

  Translation of Icelandic text in the image: Reiknitími - Initialization time. Time when the forecast was prepared Gildistími - Validation time. Time when this forecast image is valid klst - hour An Atlantic ocean forecast is based on model calculations from the European Centre for Medium-Range Weather Forecasts ECMWF /weather/forecasts/atlantic/

• 37. Wind

  Translation of Icelandic text in the image: Reiknitími - Initialization time. Time when the forecast was prepared Gildistími - Validation time. Time when this forecast image is valid klst - hour An Atlantic ocean forecast is based on model calculations from the European Centre for Medium-Range Weather Forecasts ECMWF /weather/shipping/atlantic/

• 38. Daniell_etal-2010

  and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

• 39. Reykholt-abstracts

  in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 40. Helle_Katrine_Andersen_(DANVA,_Dk)

  to a diverse landscape, where water is ”grown”, and the city is green and appealing to the citizens.  The utilities supply clean drinking water for the citizens. Clean groundwater is a sustained resource, because specific areas have been allocated to groundwater formation.  Agricultural waste is utilized without risk of polluting the aquatic environment.  In the cities and industrial areas /media/loftslag/Helle_Katrine_Andersen_(DANVA,_Dk).pdf