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Results:

• 31. BIKF_windrose_2005-2014

  observations: 13639 Calm: 1.9% Variable winds: 0.22% 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 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 25 3 43 7 55 9 69 3 58 3 49 1 74 0 82 8 70 5 47 8 44 2 40 7 41 1 52 4 51 1 41 7 38 2 36 7 32 1 29 7 29 3 29 9 37 0 39 9 44 1 35 8 32 3 21 3 /media/vedur/BIKF_windrose_2005-2014.pdf

• 32. Eriksson_2-Acceptability-of-policy

  % (2%), own reduction 18% (21%), effectiveness 17% (47%), fairness 35% (27%), acceptability 51% (49%). .42 (.43) .11 (.17) .14 (24) .58 (.50) .40 (.44) .10 (.14) .16 (.26) .17 (.16) .42 (68) .50 (48) .19 (.26) .48 (.31) .27 (.31) .17 (.14) .37 (34) Acceptability of raised tax on fuel Freedom Effectiveness Own reduction Fairness Problem awareness Personal norm Pro-env orientation Willingness /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf

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

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 34. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 35. VI_2020_008

  nearest grid-points. ................................................................................................................... 47 Figure 19. IDF curves for stations Höfn í Hornafirði and Neskaupstaður comparing results based on observations to results based on ICRA simulations obtained for the same time period. ..... 51 Figure 20. 10-year return period normalised IDF curves stacked for all /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 36. News

  News © Examples from the weather app /about-imo/news/bigimg/2812

• 37. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 38. Bárðarbunga 2014 - November events

  on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 caldera earthquakes since 10:00 AM yesterday, five exceeded magnitude 4. Overall, seismicity /earthquakes-and-volcanism/articles/nr/3023

• 39. Bardarbunga-2014_November-events

  earthquakes have been detected within Bárðarbunga. Most of the recorded seismicity occurred on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 /media/jar/Bardarbunga-2014_November-events.pdf

• 40. Bárðarbunga 2014 - November events

  on the northern side of the volcano's caldera. Hardly any earthquake activity was detected along the dyke intrusion. The largest detected earthquake since yesterday's report registered magnitude 4.5. This earthquake occurred at 01:51 today on the northern side of the caldera, see earthquake maps. Of the 40 caldera earthquakes since 10:00 AM yesterday, five exceeded magnitude 4. Overall, seismicity /earthquakes-and-volcanism/articles/nr/3023/