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  • 1. Group5-Stakeholders_analysis

    - - Industries Private Strong Market Water supplier Public Strong Market Farmers (pro-nitrate group ) Private Strong Market General public Private Weak - Pro-environmental group private Medium Governance Mitigation/adaptation consultants Private Medium Market/governance 2 /media/loftslag/Group5-Stakeholders_analysis.pdf
  • 2. VED_AnnualReport-2013_screen

    in the field of volcanology have been employed to work on improving the infrastructure and services for volcano monitoring. We have actively participated in international research projects in collaboration with the Univer- sity of Iceland, the Icelandic Civil Protection Agency and several Icelandic companies. We have received considerable international funding for these pro- jects. As part /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
  • 3. IMO_AnnualReport2014

    and surveillance of earth, water and air showed its strength and was in particular very helpful in the pro vision of gas-distribution forecasts for the public. All divi- sions of IMO contributed to the e?ort which was carried out in close co-operation with the University of Iceland and the Civil Protection in Iceland, with great backing from our ministry and the government. It is not enough /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 4. Eriksson_1-Risk-perception

    Risk perception Louise Eriksson Department of Social and Economic Geography Umeå University Overview 1. Risk perception (including environmental risk perception and beliefs about climate change) 2. Environmental risk perception (problem awareness) and pro-environmental behaviours 3. Coping with the effects of climate change 2 3 (1) Risk perception • Risk is often defined as a combination /media/loftslag/Eriksson_1-Risk-perception.pdf
  • 5. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 6. Refsgaard_etal-2007-Uncertainty-EMS

    to arrive at a robust deci- sion. As with the other steps, the quality of the results needs to be assessed through internal and external reviews that also provide platforms for dialogues between water man- ager, modeller, reviewer and, often, stakeholders/public. Fig. 1 shows the key actors in the water management pro- cess and the above five steps in the modelling process. The interactions between /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 7. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 8. GA_2009_91A_4_Andreassen

    the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 9. VI_2014_005

    in 2-m temperature shown in Figure 6. Temperatures at 2 mAGL, as determined by SURFEX, can be compared with 2-m temperatures determined directly from HARMONIE, by linearly pro- jecting from the lowest two model levels. The lowest model level (L65) has an average height above ground of 11.9 m in January, and 12.2 m in July. The second lowest model level (L64) has an average height of 35.9 m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 10. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

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