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• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Volcanic plumes and tephra

  the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks and be advected far away by the wind. This fraction of the pyroclastic material can possibly generate a distal deposit very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d /volcanoes/volcanic-hazards/volcanic-emissions/

• 3. FAQ

  and be advected far away by the wind. This fraction of the pyroclastic material can possibly generate a distal deposit very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d < 64 mm Ash d < 2 mm Fine ash d < 0.063 mm Table 1 Terminology of pyroclast material and its size.At ground level volcanic tephra can cause: Health issues; Roofs/building collapse; Poor visibility /volcanoes/grimsvotn-activity/faq/

• 4. VI_2020_004

  ......................................................................................................................... 41 5.2.1 Input parameters and synthetic scenario .......................................................... 41 5.2.2 Validating model results with real deposit map ............................................... 43 5.2.3 Probabilistic hazard maps /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 5. VI_2020_011_en

  An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, Jacopo Selva, Simone Tarquini, Mattia de´Michieli Vitturi, Ingibjörg Jónsdóttir, Davið Egilson /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 6. Publications 2020

  assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, o.fl. 73 16,0 2020-008 Reassessment of precipitation return levels in Iceland Andréa-Giorgio R. Massad, Guðrún Nína /about-imo/publications/2020/

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

  power delivery Finances and risk Financial resources concentrated in structural protection (sunk costs) Financial resources diversified using a broad set of private and public financial instruments Climate change adaptation in European river basins 267 123 Tabl e 2 Overvie w o fvariable s an d indicator s fo rAIW M Dimensio n Variabl e Indicato r Literatur e (A )Agenc y 1. Typ e o fleadershi p /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 8. VI_2014_001

  frequency distributions for Re- gion 1 derived with index flood model no. 6: bµ(D) = a(AP=Z)b ............................ 39 5 Appendix VI - Empirical and modeled daily flood frequency distributions for Region 2 derived with index flood model no. 3: bµ(D) = a(APm)b ......................... 41 Appendix VII - Instantaneous Index flood models for Region 1. .......................... 43 Appendix VIII /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 9. VI_2015_009

  presents the study area and data. Sec- tion 3 describes the methodology. Section 4 presents the results and Section 5 concludes the report. 2 Study area and data 2.1 River basins Rivers in Iceland are often classified according to the origin of flow (Rist, 1990): direct runoff (D), spring-fed (L), glacier-fed (J) and whether they flow through lakes (S). Twelve river basins were selected for this study /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 10. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  requires an appropriate monitoring system and the use of integrated or more simple models for the prediction of future scenarios including effects of implemented measures. Such integrated models should also include socio-economic aspects. In the Netherlands for the Major sources of uncertainty in current IWRM practice Tabl e 1 St ep 1: Es ta bl ish st at us an d go al s Pr oces s in Ste p 1 Es tablis /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf