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• 31. 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

• 32. 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

• 33. Kok_JGEC658_2009

  ) describes a 10-step approach where narrative storylines are developed and linked to dynamic models in an iterative procedure. Stories are developed by a stakeholder panel consisting of the relevant actors in the region under study, while models are developed and applied by experts. Examples of global exercises that have used an approach similar to Story-and- Simulation include the Millennium /media/loftslag/Kok_JGEC658_2009.pdf

• 34. 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

• 35. VI_2016_006_rs

  of W-Strandartindur and the gullies below .................................................................................................. 23 4.5 Areas 7 and 8: Botnabrún ........................................................................ 24 4.6 Areas 9 and 10: Nautaklauf and Klauf ........................................................ 24 5 Assessment of the hazard potential /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. 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

• 37. VI_2014_006

  The analogue method.............................................................................. 9 2.2.1 Principle and background .............................................................. 9 2.2.2 Prerequisites............................................................................... 10 2.2.3 Predictors .................................................................................. 11 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 38. Observations - Þverfjall II

  Observations - Þverfjall II | Observations | Icelandic Meteorological office Observations - Þverfjall II Mon 1.05 14 GMT E 10 Max wind : 10 / 12 13 GMT E 9 Max wind : 10 / 11 12 GMT E 9 Max wind : 9 / 10 11 GMT E 8 Max wind : 10 / 12 10 GMT ENE 9 Max wind : 10 / 12 09 GMT ENE 8 Max wind /m/observations/areas

• 39. Session program Thursday 13. October

  08:30 – 10:10 Oral session - Chair: Martin Hensch 08:30 – 08:50 Ambient noise tomography of Eyjafjallajökull Ásdís Benediktsdóttir, Ólafur Guðmundsson, Bryndís Brandsdóttir 08:50 – 09:10 Long-period earthquakes recorded on a dense seismic array during the 2014 Bárðarbunga rifting event Bryndís /norsem/norsem2016/program/thursday

• 40. Session program Wednesday 12. October

  08:30 – 10:00 Opening and oral session - Chair: Páll Einarsson08:30 – 08:45 Opening address Kristín S. Vogfjörð, Kristín Jónsdóttir, Martin Hensch08:45 – 09:00 Nordic collaboration and contribution to the European Plate Observing System - EPOS Kristín Vogfjörð 09:00 – 09:20 Seismic /norsem/norsem2016/program/wednesday