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Results:

• 21. Bardarbunga-2015_MarchAprMay-events

  by the Institute of Earth Sciences in mid March, the Icelandic company Svarmi ehf filmed the Holuhraun lava field, using drones. The results are now available on their web-site, including: A striking 5 min. video showing a 3D model of the newly formed craters in Holuhraun (Svarmi ehf). 24 April 2015 - the Aviation Colour Code now green IMO has changed the Aviation Color Code for the Bárðarbunga /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 22. VI_2015_007

  distribution and parameter estimation method The Generalized Extreme Value (GEV) distribution (Jenkinson, 1955) was adopted to model the flood frequency distribution from the AMF series: Qi(D;T ) = ei + ai ki (1 [ ln(1 1=T )]ki) if ki 6= 0 ei ailn( ln(1 1=T )) if ki = 0 (7) where ei is the location parameter, ai is the scale parameter and ki is the shape parameter. The method of probability weighted /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 23. VI_2014_005

  model errors discussed in the previous section, a model time-series of 2-m temperature or 10-m wind speed, Mi(t), interpolated to the i-th station location, can be linearly transformed such that the mean square error compared with the local station time-series is minimised. Generally, the corrected time-series is then given by M˜i(t) = ai Mi(t)+bi ; (2) where at each station location, the correction /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 24. 2005EO260001

  At 2250 UTC, the plume was detected by the weather radar at ~8 km height over Vatnajökull, reaching ~12 km four hours later (Figure 1c). Lightning over Grímsvötn, which accompanied the rising plume (Figure 3d), was eventually seen at ~0300 UTC, but darkness and weather conditions prevented visual observation of the eruption site until the following day. Over the next two days, the strength /media/jar/myndsafn/2005EO260001.pdf

• 25. Hare-2011-ParticipatoryModelling

  Simulatio n mode l (scientific ) Im pr o ve m o de l (quality ) Fa rm er s, Fa rm busines s advisor sNO P IN D Interview s NO P IN D Qu es tio n n ai re – verificatio n NO P OT :Researcher s M KA/ M M (re nements ) KA M Has e I Simulatio n mode l (scientific ; discussio n su pp o rt ) Im pr o ve m o de l (quality , acceptance ) Farmers ,loca l authorities , association s IN D Reques t fo rdat a N /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 26. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 27. IMO_AnnualReport2014

  probably a few meters. An interactive 3D model of the earthquakes during the magma intrusion. The di?rent colours represent the activity in time from 16 August to 12 September. During the magma intrusion, intense earthquake activity related to subsidence of the Bárðarbunga caldera was located at the caldera rim. Over 70 earthquakes above magnitude 5 occurred in the first four months after the onset /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 28. ces_geus_paakitsoq_full_report

  in winter(Fig. 3d). Standard deviation of monthly mean Ta are in reasonable agreement to the observations except for summer and autumn on the ice sheet where the model underestimates (Fig. 4c and d). 5.2 Global Radiation Measurements of global radiation are only available from the stations Swiss Camp and Crawford on the ice sheet for a limited time period (1995–2006), including a number of data gaps /media/ces/ces_geus_paakitsoq_full_report.pdf

• 29. Refsgaard_2-uncertainty

  6 – Nordjylland 9934 47649 Omr. 7 – Bornholm 2358 10106 DK-model - The hydrological model Model code MIKE SHE/MIKE11 • 3D groundwater flow • 2D overland flow • Drain flow (pipes, ditches) • 1D river routing • 1D unsaturated zone, Two- layer module (evapotranspiration) • Degree-day snow melt/accumulation •Borehole data •Geological interpretation •Incorporation of knowledge from more than 50 /media/loftslag/Refsgaard_2-uncertainty.pdf

• 30. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf