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  • 51. Bárðarbunga 2015 - February events

    hazards group of the Institute of Earth Sciences. 26 February 2015 10:00 - from geoscientist on duty Over ten earthquakes have been observed in Bárðarbunga past 24 hours. All the quakes were below magnitude 1.4. Also over ten quakes observed in the dike intrusion and all below magnitude 1.4. Two quakes observed in Tungnafellsjökull, the larger one of magnitude 1.7. Seven quakes were observed /earthquakes-and-volcanism/articles/nr/3087/
  • 52. Bardarbunga-2015_February_events

    observed in Tungnafellsjökull, the larger one of magnitude 1.7. Seven quakes were observed in Askja, the largest of magnitude 2.3 at 05:42 last night. At Herðubreið three quakes were observed all below magnitude 2. 25 February 2015 10:00 - from geoscientist on duty Since yesterday morning over 20 earthquakes were observed in Bárðarbunga. The largest were of magnitude 1.7. In the dike intrusion /media/jar/Bardarbunga-2015_February_events.pdf
  • 53. Bardarbunga-2015_January-events

    Another quake of magnitude 4.6 occurred in the southern caldera rim at 15:00 yesterday. In total, seven quakes were registered of magnitude 4.0 to 4.6. Almost 15 quakes were observed in the dike intrusion, all below magnitude 2. Also about 15 quakes were observed in Tungnafellsjökull, the largest of magnitude 3.1 at 13:17 yesterday. 13 January 2015 - from the Scientific Advisory Board Notes from /media/jar/Bardarbunga-2015_January-events.pdf
  • 54. Bardarbunga_kafli20140825

    Over the last seven years seismic activity has been gradually increasing in Bárðarbunga and the northern part of the fissure swarm. This activity dropped again after the Grímsvötn eruption in May 2011, but it soon began to increase gradually again. In May 2014, there was a relatively small swarm of over 200 events. An intense seismic swarm started under the eastern part of Bárðarbunga system /media/jar/Bardarbunga_kafli20140825.pdf
  • 55. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

    2009/2010 Introduction Central Denmark Region has participated in seven workshops and identified climate change challenges faced by society in relation to water and water resources: The project is called "Climate in Practice" The project will inform the municipalities and businesses based in Central Denmark Region about the local impact of climate change on water and water resources /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
  • 56. Case_A___Horsens_Fjord

    Introduction Central Denmark Region has participated in seven workshops and identified climate change challenges faced by society in relation to water and water resources: The project is called "Climate in Practice" The project will inform the municipalities and businesses based in Central Denmark Region about the local impact of climate change on water and water resources. Furthermore /media/loftslag/Case_A___Horsens_Fjord.pdf
  • 57. Horsens_case

    /2010 Introduction Central Denmark Region has participated in seven workshops and identified climate change challenges faced by society in relation to water and water resources: The project is called "Climate in Practice" The project will inform the municipalities and businesses based in Central Denmark Region about the local impact of climate change on water and water resources. Furthermore /media/loftslag/Horsens_case.pdf
  • 58. Refsgaard_2-uncertainty

    of rainfall days No change in distribution of rainfall intensity Etc. Seven sub-models –Horisontal discretization: 500 m –Vertical discretization – layers, varying numbers and geometry Delmodel Samlede landareal (km2) Aktive grids pr. lag Omr. 1 – Sjælland 7163 37569 Omr. 2 – Sydhavsøerne 2042 13885 Omr. 3 – Fyn 3473 24009 Omr. 4 – Sønderjylland 7897 35869 Omr. 5 – Midtjylland 11578 49993 Omr /media/loftslag/Refsgaard_2-uncertainty.pdf
  • 59. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    and Action Plan (6) ? IWRM framework ? IWRM leadership ? River basin action plan Fig. 2 The seven different steps with their main processes in the IWRM cycle (modified after Jønch-Clausen 2004). The numbers in parenthesis denote the step 1–7 P. van der Keur et al. formulated through learning from previous implemented strategies. This can be achieved by iteratively comparing new adaptation /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 60. ces-oslo2010_proceedings

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