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• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. WAFC Prognostic charts

  Office: Valid: Analysis 00 z 06 z 12 z 18 z Forecast 00 z 06 z 12 z 18 z SIGWX charts: Valid: NAT 00 z 06 z 12 z 18 z EUR 00 z 06 z 12 z 18 z EUR wind forecast charts NAT wind forecast charts Tropopause - height and temperature Max wind and FL Humidity /weather/aviation/wafc/

• 3. SIGWX Map

  Contact IMO © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 | SSN 630908-0350 Contact us | Employees | Terms and conditions | Sitemap Other related web sites Icelandic Mobile web /weather/aviation/sigwx/

• 4. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208

• 5. Glossary

  We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/

• 6. Poster presentations

  on Intraplate Seismicity in Central Fennoscandia Annakaisa Korja, Uski, M., Lund, B., Grigull, S., Nironen, M., E., Högdahl, K. Relative earthquake location in Southern Iceland Bergþóra S. Þorbjarnardóttir and Ingi Þ. Bjarnason This year's update on the Burträsk fault seismicity Darina Buhcheva and Björn LundThe SIL-system from an operational standpointJón Söring Communication between /norsem/norsem2016/program/poster

• 7. norsem_schmidt

  using Seiscomp3 and a virtual global network of stations, made available to us either directly from collaborating institutes or via IRIS and GFZ, as well as event parameters published by EMSC and USGS. After the initial alert, event parameters and classification are continuously updated as more data on the event becomes available. Being automated and targeted at early warnings, the system /media/norsem/norsem_schmidt.pdf

• 8. Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik

  Impacts of Climate Change on Stormwater Systems in Reykjavík Ásta Ósk Hlöðversdóttir1*, Philippe Crochet2, Jónas Elíasson1, Hrund Ó. Andradóttir1 and Brynjólfur Björnsson3 1 University of Iceland, 2 Icelandic Meteorological Office, 3 Mannvit Engineering *Corresponding author. Email address: aoh3@hi.is Due to climate change, precipitation is projected to increase in Northern Europe (Bates /media/loftslag/Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik.pdf

• 9. 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

• 10. VI_2014_001

  flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf