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• 1. News

  of Ólafsvík is to the left. The fracture line of the avalanche on 19 March 2012 is visible near the top of the slope to the right in the photograph and the avalanche tongue extends to the foot of the slope below the fracture line (this is where the lower part of the hillside is whiter than elsewhere). The fracture line extends into the supporting structures at the location of the topmost row and extends /about-imo/news/bigimg/2476

• 2. Articles

  of Ólafsvík is to the left. The fracture line of the avalanche on 19 March 2012 is visible near the top of the slope to the right in the photograph and the avalanche tongue extends to the foot of the slope below the fracture line (this is where the lower part of the hillside is whiter than elsewhere). The fracture line extends into the supporting structures at the location of the topmost row /avalanches/articles/bigimg/2475

• 3. 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

• 4. Instructions on using Atlantic Ocean forecasts

  isobars signify the air pressure, in millibars, at the ocean surface (1 mb = 1 hPa). The red, purple and blue isotherms show the temperature at 2 m above the ocean surface. A blue line denotes sub-freezing conditions; a purple line denotes 0°C and; a red line denotes temperatures above freezing. Wind speed is displayed in metres per second (m/s). The angle of the wind barb is indicative /weather/articles/nr/1218

• 5. Adalgeirsdottir-etal-tc-5-961-2011

  and thinning during the 20th century. The radio-echo sounding (RES) line network and sites of RES point survey is shown in (E). The red line is the 2001 ice divide for Hoffellsjökull (212 km2). The most accurate glacier DEM is created from the air- borne LiDAR survey conducted in the autumn of 2010 (5× 5 m pixel resolution, with an accuracy of <20 cm in el- evation and <0.5 m in position, Fig. 3). It is used /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 6. 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

• 7. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 8. 47th Nordic Seismology Seminar

  September 23:59 UTC.Abstracts shall be sent in email as plain text to: ingibjorg@vedur.is For the subject line, please adhere to: "NordSem 2016 Abstract [name of main author]"Please provide the following information:TitleNames of all authors (indicate who is presenting if not first author)Affiliations of all authorsAbstract text (we do not have a restriction on the maximum number of words /norsem/norsem2016/abstract-submission/

• 9. News

  located at Keflavik International Airport, at 220 km distance from the volcano. The cloud extends above a large part of Vatnajökull ice cap. The line marks the approximate location of Grímsvötn volcano. News 2023 2022 2021 2020 2019 2018 /about-imo/news/bigimg/2174

• 10. Trausti_Jonsson_(IMO,_Ice)

  of large natural events in the 1960s and early 1970s showed that this line of thought was at the best wrong, but possibly also dangerous. Since then the need for natural hazard management in the broad sense has become more and more obvious in Iceland. The assessment of Icelandic natural hazards fit very well into the frame proposed by the WMO at the end of the International Decade for Natural /media/loftslag/Trausti_Jonsson_(IMO,_Ice).pdf