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  • 51. Mid-Latitudes-Agenda1_nov2013EH

    Agenda *All presentations will be in the Forgardur (forecourt) underground basement room of the IMO building at Bustadavegur 7, unless otherwise noted. Wednesday, 13 November Time Agenda Item 09:00 – 09:15 Welcome and Introductions - T Jónsson and E Hanna 09:15 – 09:30 Meeting Structure and Overview - J Overland and E Hanna 09:30 – 10:40 09:30 – 09:45 09:45 – 10:05 10:05 – 10:25 /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
  • 52. Program

    (see below) and the list of participants in addition to the abstracts of presentations and posters. Sessions Thursday, 20 June 09:00–09:10 ‒ Welcome 09:10–10:30 ‒ Lidar measurements for glacier inventories and mass balance monitoring 11:00–12:30 ‒ Process studies – I 13:30–15:00 ‒ Process studies – II 15:30–17:30 ‒ Lidar measurements from space, incl. video discussion with input from NASA /lidar/lidar-2013/program/
  • 53. PhD_course-Programme_26Aug2011-final

    Programme Time Topic Responsible Material Sunday, August 21 Arrival Monday, August 22 9:00 - 9:30 Welcome JCR Course programme IPCC (2007) 9:30 - 10:30 Introduction to adaptive management HJH Milly et al. (2008) Huntjens et al. (2010) Henriksen and Barlebo (2008) Coffee 10:45 - 13:300An introduction to participatory methods and to planning participatory processes MH Processes: Moellenkamp /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
  • 54. 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
  • 55. 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
  • 56. 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
  • 57. 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
  • 58. Refsgaard_etal-2007-Uncertainty-EMS

    and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 59. VI_2009_006_tt

    to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 60. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

    at the operational/local level. A calibrated approach (standardized questionnaires and interviews, expert judgment, and reinterpretation of out- comes by means of relevant literature) was used to com- pare the state of affairs in water management in the selected case-studies. Adaptive and integrated water management Given the expected increase of climate-related extreme events, water governance capabilities /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

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