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Results:

• 11. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 12. IPPC-2007-ar4_syr

  Pateh Jallow, Luc4ka Kajfez4-Bogataj, Neil Leary, Hoesung Lee, David Wratt Climate Change 2007: Synthesis Report Synthesis Report An Assessment of the Intergovernmental Panel on Climate Change This underlying report, adopted section by section at IPCC Plenary XXVII (Valencia, Spain, 12-17 November 2007), represents the formally agreed statement of the IPCC concerning key findings /media/loftslag/IPPC-2007-ar4_syr.pdf

• 13. Journal_of_Hydrology_Veijalainen_etal

  ; fax: +358 20 490 2590. E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen). Journal of Hydrology 391 (2010) 333–350 Contents lists available at ScienceDirect Journal of Hydrology journal homepage: www.elsevier .com/ locate / jhydrol Author's personal copy narios from GCMs or RCMs, and with different emission scenarios (e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 14. VI_2020_005

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2 Background . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.1 Factors affecting sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.1 Main factors affecting sea level in Scandinavia, the UK and Iceland . . . . 13 2.2 Sea level data /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 15. Adalgeirsdottir-etal-tc-5-961-2011

  from this run are shown in Fig. 12. that best simulated the measured glacier geometry. The rate factor (A) calibrated in this manner is on the order of 6× 10−15 s−1 kPa−3; a value that has been recommended for temperate ice (Paterson, 1994), but characterizes softer ice than the average of a series of model calibrations that is now recommended (Cuffey and Paterson, 2010). Here, two ap- proaches /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 16. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

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

  Grin’s work on this article was part of the programme of the Dutch Knowledge network on System Innovations (KSI). P. Huntjens (&)  C. Pahl-Wostl Institute for Environmental Systems Research, University of Osnabruck, Barbarastraße 12, Geb. 66, 49069 Osnabruck, Germany e-mail: patrickhuntjens@yahoo.com J. Grin Amsterdam School for Social Science Research, University of Amsterdam, Amsterdam /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 18. 2010_005_

  in hectopascals during the 1961–90 control period, for the reanalyses and the RCMs. . . . . . . . . . . . . . . . . . . 32 11 Dependence on terrain elevation of linear trends of total precipitation within the 2004–50 period in the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5, together with the corresponding model orographies. . . . . . . . . . . . . . . . . . 33 6 12 Mean annual total precipitation /media/ces/2010_005_.pdf

• 19. VI_2015_009

  principle ................................................................................... 11 3.2 Flood frequency distribution and parameter estimation method ........................ 12 3.3 Evaluation statistics ................................................................................ 12 4 Results /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 20. VI_2015_005

  and precipitation....................... 12 5 Coefficient of determination between pressure and zonal wind ......................... 13 6 Daily fields of pressure and 850 hPa geopotential height................................. 14 7 Seasonal cyclone occurrence on different timescales ...................................... 17 8 Seasonal occurrence of low-pressure centres, as a function of centre /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf