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• 21. 2013_001_Nawri_et_al

  ] 1000 1006 1012 T0 [ C] 1 5 9 LT [K km 1] 7.1 6.3 5.1 L [K km 1] 2.6 5.7 7.9 within that part of the island with terrain up to 1000 m above mean sea level (mASL). The expo- nential decrease in pressure with height outweighs the linear decrease in temperature, leading to an effective decrease in air density with height. The standard value of 1.225 kg m 3 is therefore only appropriate at low /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 22. VI_2015_005

  but are considered for climatological anal- yses only if their centre depression on the 1000 hPa geopotential height field reaches at least 20 m relative to the 24 surrounding grid points over the course of their lifetime. 7 This study is concerned with well-developed, persistent, mid- to high-latitude large-scale weather systems, rather than their early detection and tracking. Therefore, cyclones /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 23. Climate Report

  from 9°C on the east coast to 16°C in the interior in north-eastern part of Iceland. Precipitation is highest in the glaciated highlands of south Iceland with annual values in excess of 5000 mm of annual accumulated precipitation on the highest glaciers and in general with high values ranging from 1000 mm up to 3000 mm in mountainous areas. Lower values with less than 1000 mm prevail north /climatology/iceland/climate-report

• 24. Climate Report

  from 9°C on the east coast to 16°C in the interior in north-eastern part of Iceland. Precipitation is highest in the glaciated highlands of south Iceland with annual values in excess of 5000 mm of annual accumulated precipitation on the highest glaciers and in general with high values ranging from 1000 mm up to 3000 mm in mountainous areas. Lower values with less than 1000 mm prevail north /climatology/iceland/climate-report/

• 25. aerodrome_summaries_20140603

  ) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME (UTC) <800 <1500 <3000 <8000 <200 <500 <1000 <2000 0 1 1 3 9 1 1 2 3 9 2 1 2 3 9 3 1 2 3 9 4 1 2 3 9 5 1 2 3 9 6 1 2 3 9 7 1 2 3 9 8 1 1 3 9 9 1 1 3 9 10 1 1 3 9 11 1 1 3 /media/vedur/aerodrome_summaries_20140603.pdf

• 26. VI_2009_002rs

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf

• 27. Pollution

  and a river close to the site and a lake nearby. Elevation is 65 m above sea level, distance from the sea is 26 km and distance to towns of about 1000 inhabitants is about 15 km. This is an ideal inland background station at 64oN 21oW. Since 1980, daily sampling has been done at Írafoss, monitoring sulphur concentrations and related substances. In fact, daily sampling was done at Rjúpnahæð /pollution-and-radiation/pollution/

• 28. Alam_Ashraful_CES_2010

  Dominant height (m) Basal area just after thinning area threshold 60 80 100 120 Energy wood (Mg ha-1) 60 80 100 120 60 80 100 120 17 Findings: ecosystem CO2 balance 548.4 400 600 7.8 150.4 0 200 -200 O 2 m - 2 -390.86 -600 -400 g C O 1000 -800 -1097.6-1200 - Management Litter Humus 18 Emissions Capture Balance Conclusions • Large amount of unutilised energy biomass are available in Finland • Climate /media/ces/Alam_Ashraful_CES_2010.pdf

• 29. Group3-Road-scenarios

  in five-year basis  Current state of the road network affects the possible decisions to be made at the moment Political adaptation Management structures have to be more flexible and ready to apply adaptive management Technological adaptation 0 1000 2000 3000 4000 5000 6000 1985199019952000200520102015202020252030 vans (mln. tonkm) lorries (mln. tonkm) 0 10000 20000 30000 /media/loftslag/Group3-Road-scenarios.pdf

• 30. VI_2015_006

  elevation contour lines are drawn at 1000 mASL, indicating roughly the extent of the glaciers. 15 3 Radiation fluxes at the surface With increasing time past the summer solstice (20 June 2012), the solar energy per unit area received at the Earth’s surface, for the same cloud and snow conditions, decreases due to the shorter days and lower sun altitude angles. The characteristics of the solar cycle /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf