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11. West fjords - earthquakes during the last 48 hours (Preliminary results)

12. Guidelines2-for-rapporteurs

Adaptation conference 29-31 August 2012 – Helsinki – Rantapuisto Guidelines for rapporteurs  Please report the sessions assigned to you (see table below)  You can swap sessions with another rapporteur, if the concerned rapporteur explicitly affirmed that swap and no other time or task conflicts occur (this is to be checked with the co-chair who coordinates rapporteur slots – Adriaan /media/loftslag/Guidelines2-for-rapporteurs.pdf

13. Publications 2012

flood frequency analysis in northern Iceland Philippe Crochet 55 pp 1,7 Mb 2012-011 Statistical Correction of WRF Mesoscale Model Simulations of Surface Wind over Iceland based on Station Data Nikolai Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 26 pp 1,1 Mb 2012-010 Evaluation of WRF Mesoscale Model Simulations of Surface Wind over Iceland Nikolai /about-imo/publications/2012/

14. Sea ice in February 2009

2009 Sea ice in February 2009 In the beginning of February satellite information showed that sea ice was about 55 nm /sea-ice/monthly/2009/nr/2324

15. Staff members

Meteorologist Service and Research Division Anton Berg Carrasco Snow avalanche observer /about-imo/employees/

16. News

at the eastern margin of Skeiðarárjökull and the mountains in the background are Krossgilstindur (near) and Færnes (further). The event is a glacier outburst flood in river Gígjukvísl. However, the photo shows the river outlet of Skeiðará, which changed its course in 2009 and now runs due west along the margin of Skeiðarárjökull outlet glacier and contributes to Gígjukvísl, see map from ja.is /about-imo/news/bigimg/2859

17. aerodrome_summaries_20140603

CLIMATOLOGICAL SUMMARY - TABLE A AERODROME: BIAR - AKUREYRI / Akureyri PERIOD OF RECORD: 2001–2010 LATITUDE: 65 39’31"N LONGITUDE: 18 04’20"W ELEVATION ABOVE MSL: 3 M (9FT) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME /media/vedur/aerodrome_summaries_20140603.pdf

18. ces-oslo2010_proceedings

change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

19. A strong earthquake

of Selfoss which is a town 55 km east of Reykjavík. This area is referred to as Ölfus. The bridges across river Ölfusá were closed temporarily for routine safety precautions. Please use our enquiry form to report any observations of the earthquake and its effects. Take care to mention location and timing also. Ölfus is in the so called south Iceland seizmic zone where earthquakes are to be expected /about-imo/news/nr/1305

20. The crater at Grímsvötn

and at Skrokkalda located 50 west of the eruption. Water is clearly seen in the fissure (photo below). The eruptive activity is now concentrated at two small vents surrounded by a thin circle of tephra. The eruption plume drifted slowly southwards but ash fell down from the plume into a brownish layer of ash which spread out over southern Iceland beneath a steady layer of air, located at 2-3 km height a.s.l /about-imo/news/nr/2188

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