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Results:

• 11. 2011_005

  in Appendix III. 4.2 Preferred layout of the network The Iceland CGPS network has been installed mostly through research grants of different projects with various collaborators. As a result the network coverage is uneven around the country. Areas outside of the active plate boundary have hardly any GPS stations and the network coverage is lacking for large part of the plate boundary, many /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 12. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 13. 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

• 14. Lidar 2013

  measurements are in widespread use for mapping changes of ice sheets and glaciers. With developments in unmanned aerial vehicles (UAVs) and terrestrial lidar, and novel photon counting techniques for both airborne and satellite applications, lidar measurements will continue to be a key tool for ice sheet and glacier monitoring, and measurement of sea ice properties. The 2-day workshop is aimed to bring /lidar/lidar-2013

• 15. Lidar 2013

  measurements are in widespread use for mapping changes of ice sheets and glaciers. With developments in unmanned aerial vehicles (UAVs) and terrestrial lidar, and novel photon counting techniques for both airborne and satellite applications, lidar measurements will continue to be a key tool for ice sheet and glacier monitoring, and measurement of sea ice properties. The 2-day workshop is aimed to bring /lidar/lidar-2013/

• 16. Participants

  Directorate (NVE), Norway Neil Arnold, Scott Polar Research Institute (SPRI), University of Cambridge, England Joaquín Muñoz-Cobo Belart, University of Iceland, Iceland Beata Csatho, University of Buffalo, USA Mauro Fischer, Department of Geosciences, University of Fribourg, Switzerland René Forsberg, DTU Space, Technical University of Denmark Sverrir Guðmundsson, Institute of Earth Sciences /lidar/lidar-2013/participants/

• 17. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  can be found in Huntjens et al. (2007), Chapter 4 of NeWater Deliverable 1.7.9a (http://www.newater.info). Climate change adaptation in European river basins 265 123 interactions, by private and public actors, to achieve adaptation and to enhance the capacity of processes, institutional arrangements and actors to adapt to future environmental changes (Huitema et al. 2009). Adaptive governance /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 18. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf

• 19. Other institutions

  Space Agency ESA National/Naval Ice Center's website The Cryosphere Today - University of Illinois National Snow and Ice Data Center - NSIDC Polar Data Catalogue - Canadian Cryospheric Information Network Related content /sea-ice/webs/

• 20. Lorenzoni_Pidgeon_2006

  for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf