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  • 51. 2010_005_

    such as land-sea differences and changes with terrain elevation, as well as seasonal differences. Additionally, the impact of driving GCMs on RCM runs will be investigated. 2 Data and Methodology Data used in this study are monthly fields of surface (2m) air temperature (SAT) and total precipi- tation (TP), obtained from global as well as regional climate simulations. The global data sets are 20th /media/ces/2010_005_.pdf
  • 52. VI_2013_006

    are published on the web, as a map, graph and tables. The text and labels are in Icelandic, but an English glossary is provided. The web site is currently: http://brunnur.vedur.is/athuganir/eldingar/eldgos/ The main page shows a map with the lightning locations in Iceland during the past 24 hours, color coded in 3 hour bins. Detailed explanations are provided on the web. Additionally, a graph /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
  • 53. Bárðarbunga 2014 - December events

    to make loops even farther away. Enlarge. Institute of Earth Sciences. 28 December 2014 12:00 - from geoscientist on duty The two largest earthquakes in Bárðarbunga past 24 hours were of magnitude 4.6 at 14:49 yesterday and 07:23 this morning. Additionally, there were three quakes over magnitude 4 and 12 between 3 and 4. In total over 40 quakes were observed in Bárðarbunga. Four quakes were /earthquakes-and-volcanism/articles/nr/3055
  • 54. Bárðarbunga 2014 - December events

    to make loops even farther away. Enlarge. Institute of Earth Sciences. 28 December 2014 12:00 - from geoscientist on duty The two largest earthquakes in Bárðarbunga past 24 hours were of magnitude 4.6 at 14:49 yesterday and 07:23 this morning. Additionally, there were three quakes over magnitude 4 and 12 between 3 and 4. In total over 40 quakes were observed in Bárðarbunga. Four quakes were /earthquakes-and-volcanism/articles/nr/3055/
  • 55. Kok_JGEC658_2009

    = 0) and +0.6 (e23 = 0.5). Because the value of C2 decreasesmore rapidly in the second case, the negative impact on C1 is less, as a result of which C1 stabilises at a higher value. This example thus also shows how even in very simple systems relationships can have strong indirect effects. Additionally, it shows how linear feedbacks can produce dynamics that are strongly non-linear. The ability /media/loftslag/Kok_JGEC658_2009.pdf
  • 56. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    principles: distal and proximate attitudes to risk and the role of heuristics and biases in decision-making under uncertainty. One of the immediate problems that I have encountered is that most of the studies that have been done within this field are clinical ones, with comparatively few field studies of decision-making in the day-to-day world. Additionally, planning theory has yet to engage /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 57. Bárðarbunga 2015 - February events

    intrusion, the strongest was M1.6 today at 08:24. Additionally, five earthquakes were measured around Askja and about 10 around Herðubreið. 19 February 2015 - on pulses and the time lapse between them Earthquake pulses on the caldera rim of 30-90 minutes duration, like the one observed last night, have been characteristic for the seismic activity linked to the caldera subsidence since the beginning /earthquakes-and-volcanism/articles/nr/3087
  • 58. Bárðarbunga 2015 - February events

    intrusion, the strongest was M1.6 today at 08:24. Additionally, five earthquakes were measured around Askja and about 10 around Herðubreið. 19 February 2015 - on pulses and the time lapse between them Earthquake pulses on the caldera rim of 30-90 minutes duration, like the one observed last night, have been characteristic for the seismic activity linked to the caldera subsidence since the beginning /earthquakes-and-volcanism/articles/nr/3087/
  • 59. Bardarbunga-2015_February_events

    was M1.6 today at 08:24. Additionally, five earthquakes were measured around Askja and about 10 around Herðubreið. 19 February 2015 - on pulses and the time lapse between them Earthquake pulses on the caldera rim of 30-90 minutes duration, like the one observed last night, have been characteristic for the seismic activity linked to the caldera subsidence since the beginning of the sequence /media/jar/Bardarbunga-2015_February_events.pdf
  • 60. 2013_001_Nawri_et_al

    and cold currents in the north and east. Additionally, the variable presence of sea ice, primarily northwest of Iceland during the winter months, introduces variations in surface heating of the atmosphere, as well as in the aerodynamic roughness of the ocean surface. Given these surface-related effects, vertical changes with increasing height above ground are due to the reduced impact /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

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