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Results:

• 31. VI_2022_006_extreme

  catchments in relation to CMIP5 climate scenarios . 27 5.2.1 Presentation of the climate datasets ................................................................... 27 5.2.2 Incorporation of the climate projections to the ICRA dataset ........................... 28 5.2.3 New 1M5 maps including climate projections .................................................. 31 5.2.4 New return levels /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.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. 2005EO260001

  from 5 years of continuous GPS measurements in Iceland, submitted to Journal of Geophysical VOLUME 86 NUMBER 26 28 JUNE 2005 PAGES 245–252 Eos, Vol. 86, No. 26, 28 June 2005 EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION PAGES 245, 248 Forecasting and Monitoring a Subglacial Eruption in Iceland Fig. 1. (a) Map of Iceland illustrating the location of monitoring networks discussed in the text /media/jar/myndsafn/2005EO260001.pdf

• 34. 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

• 35. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 36. Avalanche bulletin

  by a specialist at 28 Apr 13:40 GMT Avalanche bulletins for selected areas The avalanche bulletin is at a regional scale. It does not necessarily represent avalanche danger in urban areas. Southwest corner Sat Apr 29 Low danger Sun Apr 30 Low danger Mon May 01 /avalanches/forecast

• 37. Avalanche bulletin

  by a specialist at 28 Apr 13:40 GMT Avalanche bulletins for selected areas The avalanche bulletin is at a regional scale. It does not necessarily represent avalanche danger in urban areas. Southwest corner Sat Apr 29 Low danger Sun Apr 30 Low danger Mon May 01 /avalanches/forecast/

• 38. Warning - severe gale today

  gale or severe gale warning (average wind velocity 20 to 28 m/s) is in effect for all parts of Iceland today, and in Westfjords and tonight and tomorrow. Weather forecast for the next 26 hours: Today (Wednesday): East winds, 20 to 28 m/s with snow in the south and west part of Iceland, but later sleet and rain by the coast. East 18 to 28 m/s in the afternoon, strongest winds by the coast /about-imo/news/nr/3093

• 39. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 28/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 40. 2010_005_

  decade within the 2004–50 period, for the UKMO HadCM3, and the MPI ECHAM5-r3. . . . . . . . . . . . . 28 7 Mean annual surface air temperature and total precipitation during the 1961–90 control period, and linear trends within the 1958–2001 period, for the ERA-40 reanalyses. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29 8 Differences between the RCM and underlying /media/ces/2010_005_.pdf