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  • 61. Factsheet_Bardarbunga_20150227

    and no earthquake over M5.0 since January 8th.  Around 60 earthquakes were detected in the dyke during the same period. The strongest ones were measured M1.4 and M1.3. It is worth to mention that bad weather does affect the number of small earthquakes detected.  The rate of the subsidence in Bárðarbunga caldera last week was about 5 cm per day in light of the ice subsidence /media/jar/Factsheet_Bardarbunga_20150227.pdf
  • 62. Factsheet_Bardarbunga_20141107

    University of Iceland along with representatives from the Icelandic Civil Protection, the Environmental Agency of Iceland and the Directorate of Health. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar intensity.  Seismic activity in Bardarbunga continues to be strong. Since Wednesday, 5. November /media/jar/Factsheet_Bardarbunga_20141107.pdf
  • 63. Hare_1_Part2

    (causal loop modelling) Daniel, Ferrand, Hare etal AquaStress Project Cognitive mapping and Group model building • … are contrived methods • used when it is difficult for people to explain how systems work (even when they know) 1. SH individual cognitive map (causal loop modelling) Daniel, Ferrand, Hare etal AquaStress Project Cognitive mapping a108 Elicits a cognitive map representing what /media/loftslag/Hare_1_Part2.pdf
  • 64. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    and uncertainty in a practical way. The term tool (for AM) is broadly framed, which implies that tool enhancement (for AM) can have different mean- ings. Tool enhancement can guide when and how to use a certain tool in the planning cycle in relation to IWRM or the water framework directive (WFD). It can consist of structuring the tool according to a transition framework to AM e.g. from the NeWater /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 65. NONAM_1st_workshop_summary_v3

    / interaction), 4) engage / active involvement and 5) partner / co-decision making. 3. Which knowledge is needed regarding climate effects and the involved uncertainties, and how do we obtain such knowledge? Knowledge is expertise, skills, what is known, facts, information and awareness or familiarity. Uncertainty can relate to framing, emission scenario, GCM, RCM, downscaling, local /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
  • 66. VI_2019_009

    .............................................................................................. 45 5.3 Present weather ..................................................................................... 45 Appendix ......................................................................................................... 47 5 List of Figures 1 How PWD22 determines the type of precipitation. ........................................ 11 2 Number of records as a function of the height /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 67. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

    is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
  • 68. Case_A___Horsens_Fjord

    is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/Case_A___Horsens_Fjord.pdf
  • 69. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    in the preceding review sessions. The messages can be requests, critical questions, propositions for emphasis on certain topics in future research and/or implementation, educational wishes, etc. In the opening plenary session of the Adaptation Conference on Wednesday morning two PhD students (one from each group) will present the messages (max. 5 minutes each). 2 Tasks in the Conference /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 70. VI_2016_006_rs

    in Seyðisfjörður VÍ 2016-006 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Daniel Illmer, Ingenieurbüro Illmer Daniel e.U. Jón Kristinn Helgason, Icelandic Met Office Tómas Jóhannesson, Icelandic Met Office Eiríkur Gíslason, Icelandic Met Office Sigurjón Hauksson, Efla Consulting Engineers 5 Abstract Evaluation and interpretation /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

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