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

  and thinning during the 20th century. The radio-echo sounding (RES) line network and sites of RES point survey is shown in (E). The red line is the 2001 ice divide for Hoffellsjökull (212 km2). The most accurate glacier DEM is created from the air- borne LiDAR survey conducted in the autumn of 2010 (5× 5 m pixel resolution, with an accuracy of <20 cm in el- evation and <0.5 m in position, Fig. 3). It is used /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 12. Factsheet_Bardarbunga_20150130

  January 21st blue line). The graph is based primarily on measurements from surveillance flights by the ISAVIA plane TF-FMS. There is quite some uncertainty in individual measurements but there is a definite trend showing diminishing lava flow rates. The red and pink lines show the increase of the volume of the subsidence of the Bardarbunga caldera, these values are derived with similar methods /media/jar/Factsheet_Bardarbunga_20150130.pdf

• 13. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 14. Instructions on using wind, precipitation and temperature forecasts

  shows the direction of the wind, which blows toward the point of the barb. Wind-speed is symbolized by diagonal lines at the end of the barb; for instance, a short line represents 2.5 m/s, a long line 5 m/s and a triangle represents 25 m/s. Mean sea level pressure is shown in solid lines, the contour interval is 2 hPa. The sliding bar below the map is used to change the validity time /weather/articles/nr/1211

• 15. Climatological data

  Hæll from 1931 Stórhöfði from 1931 The files above are text files, showing average temperature ("medalhiti"). First select a station, then press Get. Each line in the text-file shows one year: Average temperature for each of the 12 months and then the annual average at the end of each line, in a column marked "arid". 30 years average 1961-1990 for selected stations Reykjavík /climatology/data/

• 16. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/

• 17. Increased glacial melt due to volcanic ash

  West Iceland, is a direct run off river. Fig. 4 shows the effect of low precipitation on such rivers. During a dry spell in late summer, water discharge was very low. In preceding years, it was also rather low except during the summer of 2005 (red line). The black line (2010) shows that hardly any rain fell on the drainage area last summer. Location A map which shows the location of various rivers /hydrology/articles/nr/2110

• 18. Supporting structures stopped most of an avalanche

  A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement near /about-imo/news/nr/2476

• 19. Supporting structures stopped most of an avalanche

  A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement /avalanches/articles/nr/2475

• 20. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera