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  • 61. Bárðarbunga 2014 - December events

    have occurred in the dyke intrusion. The eruption could be seen through webcams for a short while this morning but now it is snowing. No empty patch anymore = 78.6 km² A map from 12 December 2014. The lava free patch has finally been submerged, see yellow code. The lava is now 78,6 km² (78,2 km² + 0,4 km²). Enlarge. Institute of Earth Sciences. Same day, a radar image from ESA (Sentinel /earthquakes-and-volcanism/articles/nr/3055
  • 62. Bárðarbunga 2014 - December events

    have occurred in the dyke intrusion. The eruption could be seen through webcams for a short while this morning but now it is snowing. No empty patch anymore = 78.6 km² A map from 12 December 2014. The lava free patch has finally been submerged, see yellow code. The lava is now 78,6 km² (78,2 km² + 0,4 km²). Enlarge. Institute of Earth Sciences. Same day, a radar image from ESA (Sentinel /earthquakes-and-volcanism/articles/nr/3055/
  • 63. Bardarbunga-2014_December-events

    have been detected in Bárðarbunga the last 24 hours, five between M4 and M5 and ca 10 between M3 and M4. About 10 earthquakes have occurred in the dyke intrusion. The eruption could be seen through webcams for a short while this morning but now it is snowing. No empty patch anymore = 78.6 km² A map from 12 December 2014. The lava free patch has finally been submerged, see yellow code /media/jar/Bardarbunga-2014_December-events.pdf
  • 64. 2010_012rs

  • 65. VI_2020_004

  • 66. VI_2015_005

    -Series West Central East Daily (DJF) 8.7 / 3.2 (37%) 10.8 / 1.2 (11%) 11.6 / 2.6 (22%) Daily (JJA) 10.0 / 7.2 (72%) 11.9 / 2.6 (22%) 9.4 / 5.9 (63%) 5-Day RM (DJF) 6.2 / 0.8 (13%) 10.8 / 0.3 (3%) 9.9 / 0.7 (7%) 5-Day RM (JJA) 7.0 / 5.5 (79%) 10.7 / 2.0 (19%) 6.4 / 4.8 (75%) 31-Day RM (DJF) 3.2 / 0.0 (0%) 12.5 / 0.0 (0%) 9.7 / 0.0 (0%) 31-Day RM (JJA) 4.8 / 6.0 (125%) 11.4 / 1.4 (12%) 3.8 / 3.7 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 67. Kok_JGEC658_2009

    that is accessible, interpreted as the potential for deforestation. This concept is a necessary addition to capture the effect of the spatial drivers. Fig. 2. Directed graphs (upper part) and values of concepts (lower part) for the first 30 iterations of two adjacency matrices. K. Kok / Global Environmental Change 19 (2009) 122–133 125 Author's personal copy C5: Rainfall. The hypothesis is that decreasing /media/loftslag/Kok_JGEC658_2009.pdf
  • 68. VI_2009_012

    the free parameters k and K is the constant on the right hand side of (4). For a constant stress drop of ∆σ= 1 MPa and a fit of model (1) to the PGV data with g = 0.5 the parameter K is approximately 1.5. Informally speaking, we can say that the transition between near-field and far-field takes place close to 1.5 fault radii away from the epicenter. We now show why the parameter g should fulfill /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 69. vanRoosmalen_etal-2009-WRR_2007WR006760

    water model, which makes it possible to include feedback processes of the simulated changes. 2. Study Area [9] The study area is located in the western part of Jutland, Denmark, between the Jutland Ridge and the west coast (Figure 1) with an area of 5459 km2. The topography slopes gently from east to west with land surface elevations from 125 masl in the eastern part to sea level at the coast. Land /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 70. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    different interest backgrounds the situation gets complicated. D thinks that we were a bit naive as to how open people can be in a public forum or public space. We assumed that people would be free to speak their opinion, since it was a pilot project, where the task was to test a tool. But the case showed something else. Stakeholders stuck very strictly to the policy and they let only certain /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

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