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• 11. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Iceland S. Gudmundsson et al. 8 (page number not for citation purpose) Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 and speeds up the melting as well as by exposure of old thick insulating tephra layers that prevent melting. During the 2010 eruption in Eyjafjallajo¨kull volcano, cauldron-sized holes were formed in the ice in the caldera at the centre of the ice cap /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 12. vanRoosmalen_etal-2009-WRR_2007WR006760

  evapotranspiration decreased by 19% and 22% for the two catchments, showing that the increased biomass of the vegetation only partly compensated for the 30% reduction in transpiration due to stomatal closure, as a result of the higher atmospheric CO2 concentration. [8] The aim of this study is to determine the sensitivity of the hydrological system to a number of meteorological and land use factors, which /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 13. 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