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Results:

• 21. NONAM_1st_workshop_summary_v3

  was to strengthen links and exchange information among Nordic researchers and practitioners in adaptive management related to adaptation to climate change. The workshop focused on three topics: (i) What is the difference between adaptation and adaptive management; (ii) Participatory planning processes – group model building; and (iii) Uncertainty and risk assessment. The workshop was organised /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 22. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 23. CES_BioFuels_Flyer_new

  ) and changing climate (CC:CC) 1. Current climate (CU) - varying thinning regimes (0%, 15%, 30%,45%) 2. Changing climate (CC) - varying thinning regimes (0%, 15%, 30%,45%) 3. Current (CU) & changing climate (CC) - current thinning regime 4. Current (CU) & changing climate (CC) - changed thinning regimes C l i m a t e s c e n a r i o s M ea s u r e m en t s o f c l i m a t e p /media/ces/CES_BioFuels_Flyer_new.pdf

• 24. 2010_016

  of one of the working groups in the CES project is on hydropower and hydrological modelling. One of the tasks of the Icelandic part of that workgroup was to improve the application of the hydrological model WaSiM in Iceland by: i) improving the representation of groundwater by activating the model’s groundwater module; ii) improving the representation of seasonal changes in the Hamon /media/ces/2010_016.pdf

• 25. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  networks for t i Christiansen Barlebo r Voldgade 10, DK-1350 Copenhagen K, Denmark form 3 May 2007; accepted 11 May 2007 29 June 2007 www.elsevier.com/locate/jenvman  Mak manage ARTICLE IN PRESS brought together to find a solution that is adequate from multiple perspectives. This, not only requires coping with various sources and types of uncertainty, but also with the ambiguity produced /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 26. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 27. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf

• 28. Bárðarbunga 2014 - August events

  both into the Dyngjujökull glacier and the region north of the ice margin. Earthquakes have not migrated northwards during the last two days. Seismicity remains high and, since midnight, about 700 earthquakes have been detected in the region. The largest earthquakes since midnight include: (i) a magnitude 4.5 event on the northern side of the Bárðarbunga caldera at 02:35 UTC; (ii) a magnitude /earthquakes-and-volcanism/articles/nr/3000

• 29. Bardarbunga-2014_August-events

  : (i) a magnitude 4.5 event on the northern side of the Bárðarbunga caldera at 02:35 UTC; (ii) a magnitude 4.2 earthquake in the same region at 06:18 UTC; and (iii) a magnitude 5.4 earthquake on the south-eastern edge of the Bárðarbunga caldera at 07:03 UTC. During the last two weeks, several earthquakes of similar size have occurred on the edge of the Bárðarbunga caldera. These earthquakes /media/jar/Bardarbunga-2014_August-events.pdf

• 30. Bárðarbunga 2014 - August events

  both into the Dyngjujökull glacier and the region north of the ice margin. Earthquakes have not migrated northwards during the last two days. Seismicity remains high and, since midnight, about 700 earthquakes have been detected in the region. The largest earthquakes since midnight include: (i) a magnitude 4.5 event on the northern side of the Bárðarbunga caldera at 02:35 UTC; (ii) a magnitude /earthquakes-and-volcanism/articles/nr/3000/