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  • 51. Mid-Latitudes-Agenda1_nov2013EH

    11:20 – 11:35 11:35 – 11:55 11:55 – 12:15 12:15 – 12:35 12:35 – 12:45 Jet Stream Especially the North Atlantic (Chair: Robert Erdelyi) A long perspective on Atlantic jet variability – T Woollings A comparison of North Atlantic Jet Stream Representation in ERA-Interim and 20th Century Reanalysis Data - R Hall Frozen assets: what can ships' logbooks tell us about Arctic climate change /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
  • 52. ces_flyer_glacierssnowandice

    retreated and advanced in response to climate changes that are believed to have been much smaller than the greenhouse- induced climate changes that are expected during the next decades to century. The “Hydropower, snow and ice” work group of CES will analyse the effects of future climate change on glaciers and ice caps in Nordic countries and their implications for the hydrology of glacial rivers /media/ces/ces_flyer_glacierssnowandice.pdf
  • 53. VI_2014_005

    lines). Additionally, the aver- age profiles for offshore distances to the coast of up to 30 km are shown by the black lines. For temperature, the dashed lines indicate linear projection from the two lowest model levels to 2 m above ground. A comparison of monthly averages of simulated 2-m temperature with station measurements, both for SURFEX and projected values, is shown in Figure 8. On average /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 54. 2010_005_

    Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf
  • 55. vonKorff_etal-2010

    played a role in this first phase as the author tables on decision analysis show. In summary, the comparison resulted in the reconstruction of 10 steps on which there appears to be considerable agreement among the five guides. 1. DA 1: Assemble a team for decision analysis as part of the participation design. Its members should belong to the lead agency, e.g., the water board, but can also /media/loftslag/vonKorff_etal-2010.pdf
  • 56. Bárðarbunga 2015 - March, April, May

    to reduce risk in the area will be taken and decisions on further opening of the area will then be made. The Aviation Colour Code for Bárðarbunga was changed from orange to yellow when the eruption ended. 5 March 2015 - field trip yesterday Burn out From Holuhraun lava field 4 March 2015. The photo is taken from the central part of crater Baugur, view to the North along the crater /earthquakes-and-volcanism/articles/nr/3122
  • 57. Bárðarbunga 2015 - March, April, May

    to reduce risk in the area will be taken and decisions on further opening of the area will then be made. The Aviation Colour Code for Bárðarbunga was changed from orange to yellow when the eruption ended. 5 March 2015 - field trip yesterday Burn out From Holuhraun lava field 4 March 2015. The photo is taken from the central part of crater Baugur, view to the North along the crater /earthquakes-and-volcanism/articles/nr/3122/
  • 58. Bardarbunga-2015_MarchAprMay-events

    and May. New material is added to the top of the article. In combination, the monthly articles give an overview of events: August, September, October, November, December, January, February, March-April-May and the overview article (list of links). Calendar Below is a short-cut to additions in March, April and May plus an announcement 1st June. March: 2-3-4-5-9-12-16-24-26. April: 1-3-8-11 /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf
  • 59. Twenty years of multinational earthquake prediction research in Iceland, and the future

    As in all earthquake-prone countries it has for a long time been a challenge for Icelandic seismologists to be able to warn about large earthquakes. During 1988-2005 Icelanders coordinated four international prediction research projects, with Iceland as a test-area, to build a base for earthquake warnings and better hazard assessments. The SIL project (1988-1995) was a concerted effort /earthquakes-and-volcanism/conferences/jsr-2009/earthquake-prediction/
  • 60. Grímsey earthquake swarm

    on February 16, is significantly less than the 2013 sequence, see older news, although this swarm is more steady. Continuous GPS measurements in Grímsey show no detectable deformation associated with the swarm, suggesting that the swarm is tectonic in nature although geothermal activity in the area may act as a trigger. There is no sign of magmatic activity.This area is an active seismic /about-imo/news/grimsey-earthquake-swarm

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