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  • 11. The weather in Iceland 2009

    in the East on 10th October, 185.3 mm. Snow Generally, the year had light snowfalls; the largest depth measured was at Mýri in the Northern inland on 18 January, 166 cm. The ground was totally covered by snow for 40 days in Reykjavík; this is 25 days below the long term mean. In Akureyri the ground was totally covered by snow for 97 days, 20 days below the long term mean. Precipitation days /weather/articles/nr/1802
  • 12. ved-eng-2009

    snowfalls; the largest depth measured was at Mýri in the Northern inland on 18 January, 166 cm. The ground was totally covered by snow for 40 days in Reykjavík; this is 25 days below the long term mean. In Akureyri the ground was totally covered by snow for 97 days, 20 days below the long term mean. Precipitation days Precipitation was registered on 205 days in Reykjavík, 16 days below /media/vedurstofan/utgafa/skylduskil/ved-eng-2009.pdf
  • 13. VI_2021_008

    possible. There is a constant stream of real-time seismic data coming into the monitoring office from over 80 seismometers located around the country, allowing the IMO to monitor over 30 active volcanic systems in Iceland as well as two major seismic fault zones. With the presence of so many active volcanic threats, effective monitoring and warning systems are essential. Plots of Real-time Seismic /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 14. VI_2020_004

    49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 15. Milly_etal-2008-Stationarity-dead-Science

    6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
  • 16. Bardarbunga_kafli20140825

    an 80 km2 ice-filled caldera. The characteristic activity is explosive basaltic eruptions occurring on central volcano flanks or the fissure swarm. Known eruptions have mostly been VEI 3-4 but occasionally VEI 5-6 (bulk volume of tephra up to 10 km3). The largest eruptions occurred in the early Holocene, effusive basaltic eruptions on the fissure swarm with lava volumes ≥20 km3. Eruption /media/jar/Bardarbunga_kafli20140825.pdf
  • 17. BIGJ_windrose_2005-2014

    Wind rose BIGJ 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 Frequency of wind direction (%) Aerodrome Total observations: 1324 Calm: 2.6% Variable winds: 0.23% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIGJ_windrose_2005-2014.pdf
  • 18. Sea ice in January 2011

    in the following locations: 80 nm WNW of Bjargtangar, 46 nm NW of Barði, 40 nm NW of Straumnes and 41 nm N of Kögur. No icebergs were to be seen near the ice edge. On the Greenland Strait, northeasterly wind directions were dominant to begin with, and most of the month, but at the end of the month there were a few days with southwesterly wind /sea-ice/monthly/2011/nr/2348
  • 19. Forecasts - Blönduós

    cover: 0% 15 GMT 4° NNW 6 Cloud cover: 0% 16 GMT 4° N 5 Cloud cover: 0% 17 GMT 4° N 5 Cloud cover: 50% 18 GMT 4° N 4 Cloud cover: 80% 19 GMT 4° N 4 Cloud cover: 80% 20 GMT 4° N 4 Cloud cover: 70% 21 GMT 3° NNE 3 Cloud cover: 20% 22 GMT 1° NE 2 Cloud cover: 50% 23 GMT 1° N 1 Cloud cover: 90% Wed 3.05 00 GMT 0° WNW /m/forecasts/areas
  • 20. VI_2016_006_rs

    wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

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