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Results:

• 11. 2010_005_

  period, as well as changes from the control to the 2070–99 reference period, for the reduced IPCC ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39 18 Warming by month from the 1991–2000 to the 2091–2100 period in ENSEMBLES RCMs using either the HadCM3 or the ECHAM5 as driving GCM. . . . . . . . . . 40 7 1 /media/ces/2010_005_.pdf

• 12. Wind, temperature and precipitation forecasts

  ;script type="text/javascript" src="http://vedur.is/js/iframe.js"></script> <script type="text/javascript"><!-- VI.ifrm.type = 'wel'; VI.ifrm.area = 101; VI.ifrm.lang = 'en'; VI.ifrm.displayWeather(); //--> </script> To show other areas, a different digit must be entered after 'Vi.ifrm.area'. The area codes are as follows: 101 = whole country 111 /about-imo/the-web/iframes/wind-temp-precip/

• 13. Station forecasts, text forecasts or observations

  be copied to your html file where the frame should appear: <script type="text/javascript" src="http://vedur.is/js/iframe.js"></script> <script type="text/javascript"><!-- VI.ifrm.type = 'wst'; VI.ifrm.area = 101; VI.ifrm.lang = 'en'; VI.ifrm.displayWeather(); //--> </script> To show other areas, a different digit must be entered after 'Vi.ifrm.area /about-imo/the-web/iframes/wst-txt-obs/

• 14. VI_2015_005

  This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 15. 2013_001_Nawri_et_al

  . . . . . . . . . . . . 65 36 Seasonal mean wind power density within the Skagi region . . . . . . . . . . . . . 66 37 Directional mean wind power density within the Snæfellsnes region . . . . . . . . 67 38 Seasonal mean wind power density within the Snæfellsnes region . . . . . . . . . . 68 39 Directional mean wind power density within the Þorlákshöfn region . . . . . . . . 69 40 Seasonal mean wind /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 16. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 17. VI_2020_004

  .................................................................................................................. 38 5 Results ................................................................................................................................ 39 5.1 How to read a probabilistic hazard map .................................................................... 39 5.2 Hekla /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 18. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 19. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 20. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf