Note
Volcanic eruption is ongoing on the Sundhnúksgígaröð crater row. Gas pollution hazard in the area. More

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21. Bárðarbunga 2014 - August events

August 2014 18:21 - from geoscientist on duty Few additional facts since status report earlier today: Now about 700 earthquakes have been detected since midnight. An earthquake M4.9 occurred at 16:12 on the northern rim of the Bárðarbunga caldera. The main seismic activity has been in the intrusive dike. Only a few quakes have been located near the caldera rim, mostly its nortern part. Little /earthquakes-and-volcanism/articles/nr/3000
22. Bardarbunga-2014_August-events

in Holuhraun 3rd September 2014. Photo: Richard Yeo. Updated information 31 August 2014 18:21 - from geoscientist on duty Few additional facts since status report earlier today: Now about 700 earthquakes have been detected since midnight. An earthquake M4.9 occurred at 16:12 on the northern rim of the Bárðarbunga caldera. The main seismic activity has been in the intrusive dike. Only a few /media/jar/Bardarbunga-2014_August-events.pdf
23. Bárðarbunga 2014 - August events

August 2014 18:21 - from geoscientist on duty Few additional facts since status report earlier today: Now about 700 earthquakes have been detected since midnight. An earthquake M4.9 occurred at 16:12 on the northern rim of the Bárðarbunga caldera. The main seismic activity has been in the intrusive dike. Only a few quakes have been located near the caldera rim, mostly its nortern part. Little /earthquakes-and-volcanism/articles/nr/3000/
24. Adalgeirsdottir-etal-tc-5-961-2011

). The accu- mulation zone is a part of the eastern sector of the ice cap between two mountain ranges, the subglacial Breiðabunga and Goðahnúkar, at 1350–1450 m elevation. From the ac- cumulation area, the ice flows in two branches, west and east of the central nunatak Nýju Núpar. The branches meet below the nunatak and the ice is funnelled through a 2 km wide ice fall at 600–700 m elevation where /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
25. 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
26. VI_2014_005

and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
27. VED_AnnualReport-2013_screen

as river discharge and water levels. Notices on avalanches and sea-ice are shown; short articles and news are presented. Furthermore, web and data portals can be accessed through the web, which is available in both Icelandic and English. IMO uses the social networking website Facebook for communication and feed-back. A new web-application (App) provides access to forecasts and warnings /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
28. Group4

); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf
29. vanRoosmalen_etal-2009-WRR_2007WR006760

1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn Gð Þ þ g 900T þ 273 u2 es eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d1), Rn is net radiation at the crop surface (MJ m2 d1), G is soil heat flux density (MJ m2 d1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
30. ces-oslo2010_proceedings

anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf