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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. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 33. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941

• 34. Factsheet_Bardarbunga_20140919

   Seismic activity has been rather intensive over the last 24 hours. The biggest was M5,3 at 14:21 yesterday and another one was measured M4,7 at 06:44 this morning. In total 10 earthquakes larger then M3,0 were detected in Bardarbunga since our last meeting. Smaller earthquakes were detected in Dyngjujokull glacier and in north part of the dyke.  GPS monitoring continue to show /media/jar/Factsheet_Bardarbunga_20140919.pdf

• 35. Factsheet_Bardarbunga_20141027

  over the weekend. There off 44 larger then magnitude 3,0. The biggest ones were M5,3 at 05:54 on Sunday and at 01:05 tonight.  The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as it has done over the last few weeks. Observation from air on Friday show that the depression in the caldera is 40 meters.  Geothermal heat /media/jar/Factsheet_Bardarbunga_20141027.pdf

• 36. Factsheet_Bardarbunga_20141105

  between M3 and 4. No earthquakes larger than M5 have been observed since Sunday.  The GPS station in the centre of Bardarbunga shows that the subsidence of the caldera continues with similar rate as it has been doing over the last few weeks. Measurements carried out from the air show that the greatest subsidence of the Bárðarbunga caldera has now reached 44 meters.  Energy of the geothermal /media/jar/Factsheet_Bardarbunga_20141105.pdf

• 37. Markarfljót outwash plain and Öræfajökull

  Öræfajökull Volcano: Geology and historical floods (pdf 5.43 Mb) Pages 17–44 Matthew J. Roberts og Magnús T. Gudmundsson Short summary Despite the documented severity and lasting geomorphic imprint of the 1362 and 1727 jökulhlaups from Öræfajökull, there is scant information about the routing and extent of these floods. Using field observations, aerial photographs, and modern-day analogues /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 38. Isskyrsla_20100407

  Ísskýsla 7.apríl Flug 03410.025 Miðvikudaginn 7 apríl var farið í ískönnunarflug á TF-SIF úti fyrir vestfjörðum. Kl.1115 var komið að ísröndini sem lá til NA um eftirtalda staði: 1. N65°50'- W028°05' 2. N65°44' -W027°49 ' 3. N65°56'- W027°08' 4. N66°12' -W026°21' 5. N66°31'- W025°57' 6. N66°43'- W025°49' 7. N66°40'- W025°24' 8. N67°05'- W024°32' 9. N67°14' -W023°56' 10.N67°19'- W023°32' 11.N67°40 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 39. CES_D2.4_task1

  & Dataset (ECA&D) project (Klein Tank et al. 2002; http://eca.knmi.nl/) with the global CMIP3 and regional ENSEMBLES model simulations. The selected set of stations includes nearly all Nordic (Finland, Sweden, Norway, Denmark and Iceland) stations in the ECA&D database, for which data were available for at least 44 out of the 48 years in 1961-2008. In the case of precipitation, a few stations /media/ces/CES_D2.4_task1.pdf

• 40. 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