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Results:

• 31. 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

• 32. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 33. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  & Hautala, R. 2009. Benefits and value of meteorological information services – the case of the Finnish Meteorological Institute, Meteorological Applications, 16, pp. 369–379. Meyer, M.D., Amekudzi, A., O’Har, J.P. (2009), Transportation Asset Management Systems and Climate Change: An Adaptive Systems Management Approach, paper for Transportation Research Board 2010 Annual Meeting, CD-ROM /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 34. Bio Energy

  -512. Alam, A., Kilpeläinen, A. & Kellomäki, S. (2008). Potential carbon stocks and energy production in boreal forest ecosystems under climate change responsive to varying management regimes. Submitted Biomass and Bio-energy. Kärkkäinen, L., Matala, J., Härkönen, K., Kellomäki, S. & Nuuttinen, T. (2008). Potential recovery of industrial wood and energy wood raw material in different cutting /ces/publications/nr/1939

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

  ) ESC Executive Committee Alexey Zavyalov, Russia Murat Nurlu, Turkey Mariano García-Fernández, Spain Stefano Parolai, Germany Pierre-Yves Bard, France Constantin Ionescu, Romania Stefano Solarino, Italy Steinunn Jakobsdottir, Iceland Peter Suhadolc, IASPEI Rémy Bossu, EMSC-CSEM Atilla Ansal, EAEE Bernard Dost, ORFEUS Rajender K. Chadha, ASC EUROPEAN SEISMOLOGICAL COMMISSION /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 36. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  uncertainties. Climate change impacts and adaptation also influence a wide range of stakeholders with different interests, E. Jeppesen Aarhus University, Vejlsøvej 25, DK-8600 Silkeborg, Denmark e-mail: ej@dmu.dk H. Madsen DHI, Agern Alle 5, DK-2970 Hørsholm, Denmark e-mail: hem@dhigroup.com A. Markandya BC3 Basque Centre for Climate Change, E- 48008 Bilbao, Spain e-mail: anil.markandya@bc3research.org /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 37. CES_D2.4_VMGO

  the territories of European Russia (ER) and Europe (EU) an ensemble of 9 CMIP3 [1] comprehensive global (coupled atmosphere-ocean) climate models is used in this assessment (Table 1); so called A2 scenario is considered. Both A2 and A1B scenarios are similar in terms of resulting global mean warming up to the mid-21st century IPCC [2]. The projected changes in ER and EU in many cases continue /media/ces/CES_D2.4_VMGO.pdf

• 38. 2010_003rs

  ................ 91 Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F, Brennisteinsfjöll-Bláfjöll. ................................................................................. 92 Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93 Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active between January /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 39. Bardarbunga_kafli20140825

  have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf

• 40. Hydropower - Glacier, Snow and Ice

  glacier-scaling-hydrological model. 88-89. Machguth, H., & Ahlstrøm, A. (2010). Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties. p. 42-43. Melvold, K. & Laumann, T. (2010). A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES). 90-91. Radic, V /ces/publications/nr/1940