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Results:

• 1. VI_2015_006

  6 Net downward shortwave radiation flux at the surface .................................... 18 7 Net downward longwave radiation flux at the surface ..................................... 19 8 Net downward total radiation flux at the surface............................................ 20 9 Upward sensible heat flux from the ground .................................................. 22 10 Air /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 2. 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

• 3. Observations - Holtavörðuheiði

  Observations - Holtavörðuheiði | Observations | Icelandic Meteorological office Observations - Holtavörðuheiði Mon 1.05 13 GMT -0.3° NNE 7 Max wind : 7 / 10Road temp. : 1.4° 12 GMT -1.8° NNE 7 Max wind : 7 / 10Road temp. : 0.3° 11 GMT -2.3° NNE 7 Max wind : 8 / 10Road temp. : 0.1° 10 GMT -2.8° NNE /m/observations/areas

• 4. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 5. Perrels-CBA

  Integrated • Infrastructure • Large size, indivisibilities, layers, network effects • Long lifetime, economic & spatial structuring • Public good features, implications of market organization 8/26/2011Adriaan Perrels/IL 3 26.8.2011Adriaan Perrels/IL 4 Climate change impacts – temporal profiles Duration of the state resulting from the change* Temporal profile of the unfolding of the change /media/loftslag/Perrels-CBA.pdf

• 6. Forecasts - Gufuskálar

  GMT 4° ENE 10 Cloud cover: 100% 20 GMT 3° ENE 10 Cloud cover: 100% 21 GMT 2° ENE 9 Cloud cover: 0% 22 GMT 2° ENE 8 Cloud cover: 0% 23 GMT 1° ENE 8 Cloud cover: 0% Tue 2.05 00 GMT 1° ENE 7 Cloud cover: 0% 01 GMT 1° ENE 8 Cloud cover: 0% 02 GMT 1° ENE 8 Cloud cover: 0% 03 GMT 1° ENE 8 Cloud cover: 0% 04 GMT 0° ENE 8 /m/forecasts/areas

• 7. BIHN_windrose_2005-2014

  Wind rose BIHN 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIHN_windrose_2005-2014.pdf

• 8. BIBD_windrose_2005-2014

  Wind rose BIBD 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 18358 Calm: 9.5% Variable winds: 1.7% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIBD_windrose_2005-2014.pdf

• 9. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 10. BIVM_windrose_2005-2014

  Wind rose BIVM 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 7 8 Frequency of wind direction (%) Aerodrome Total observations: 42081 Calm: 0.58% Variable winds: 3.8% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 /media/vedur/BIVM_windrose_2005-2014.pdf