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• 11. Refsgaard_etal-2007-Uncertainty-EMS

  Refsgaard a,*, Jeroen P. v Peter A. Vanroll a Geological Survey of Denmark and Greenlan b Copernicus Institute for Sustainable Development and Innovation Utrecht University, Utrecht c Environmental Modelling & Softwar equitable manner without compromising the sustainability of * Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050. E-mail address: jcr@geus.dk (J.C. Refsgaard). 1364-8152 /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 12. Staff members

  Staff members Gunnar B. Guðmundsson Job title: Seismic System Scientist /about-imo/employees/persona/25/fyrirtaeki/2

• 13. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  2007a, b). BNs were tested in a recent EU research project MERIT (Bromley, 2005; www.merit- eu.net) 2001–2004, and this tool is currently considered in Uncer wate NeWa an tainty is a central theme in integrated and adaptive r management, where different disciplines need to be Monitor and evaluate outcomes; apply learning to develop a better understanding of the system. (4) Implement policies;(3 /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 14. VI_2015_009

  (Crochet, 2012a, b; Crochet & Þórarinsdóttir, 2014) and in eastern Iceland (Crochet & Þórarinsdóttir, 2015). This study is a continuation of this work. The capacity of the IFM to estimate design floods at ungauged locations is now evaluated for river basins having substantial glacier coverage and/or substantial groundwater contribution to streamflow. The report is organized as follows. Section 2 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 15. IPPC-2007-ar4_syr

  on average sea level and on regional weather systems. It is defined here as the highest 1% of hourly values of observed sea level at a station for a given reference period. 31 Topic 1 Observed changes in climate and their effects (a) Global average surface temperature (b) Global average sea level (c) Northern Hemisphere snow cover Figure 1.1. Observed changes in (a) global average surface temperature /media/loftslag/IPPC-2007-ar4_syr.pdf

• 16. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 17. 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

• 18. VI_2014_005

  3. Differences in terrain elevation between HARMONIE model and 100-m- resolution DEM (model minus DEM): (a) original DEM interpolated onto the HAR- MONIE model grid, and (b) DEM horizontally averaged around each model grid point, using an exponential shape function with a half-width of 1 km. In addition to surface type, boundary-layer atmospheric properties are strongly influenced by the height /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 19. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 20. Alam_Ashraful_CES_2010

  scenario Summer Winter Temp ▲6˚c ▲7˚c. Precip. +10% +30% CO N l d bl2 ear y ou e 11 Forest management principles 1 ) Basal area just before thinning Thinning threshold Energy wood Energy biomass a r e a ( m 2 h a - 1 thinningt i g B a s a l a Basal area just Remaining basal area threshold Dominant height (m) after thinning 12 Management regimes Changes in basal area thinning thresholds /media/ces/Alam_Ashraful_CES_2010.pdf