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  • 1. Refsgaard_1-Welcome

    – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf
  • 2. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 3. norsem_begga

    shock mag. ~3.0 and aftershocks). The DD relocation gives tighter clustering of earthquakes in all three areas, and the strike of a fault segment, unclear in the catalog data, becomes clearly visible after relocation. Relocation shifts the centroids of the clusters by ~300 m from catalog locations, but relative distances between clusters do not change significantly. Our next step is to extend /media/norsem/norsem_begga.pdf
  • 4. Hare_1_PartINONAM

    Participatory methods and processes for adaptive management Dr Matt Hare Independent Consultant, Mexico City Adaptive and participatory water management Matt Hare, hare@gmx.de 2011 – Summer School About myself ... • Bachelor in artificial intelligence (88-92) • PhD environmental modelling in knowledge and data-poor domains (95-99) • Co-founder of Seeconsult GmbH (03-onwards /media/loftslag/Hare_1_PartINONAM.pdf
  • 5. aerodrome_summaries_20140603

    CLIMATOLOGICAL SUMMARY - TABLE A AERODROME: BIAR - AKUREYRI / Akureyri PERIOD OF RECORD: 2001–2010 LATITUDE: 65 39’31"N LONGITUDE: 18 04’20"W ELEVATION ABOVE MSL: 3 M (9FT) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME /media/vedur/aerodrome_summaries_20140603.pdf
  • 6. 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
  • 7. 2013_001_Nawri_et_al

    and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 8. 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
  • 9. 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
  • 10. Horsens_case

    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 Bygholm å and Hansted å, located in the inner part of the fjord. Several smaller streams /media/loftslag/Horsens_case.pdf

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