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• 31. 47th Nordic Seismology Seminar

  /norsem/norsem2016/accomodation/

• 32. FMI_-_Disaster_Mitigation

  a lottery. – Prior to the lottery, they could purchase “mitigation” which would protect them in the lottery. – Several rounds were performed at “hit” probabilities ranging from 1% to 20%. Hurricane Market Mitigation Study - Experimental Study Results • Market price of mitigation exceeds expected value. • Willingness to purchase mitigation increases as perceived risk increases. • Willingness /media/loftslag/FMI_-_Disaster_Mitigation.pdf

• 33. VI_2015_007

  149 S O N D J F M A M J J A l l l l l l l l l l l 0 100 200 300 15 0 25 0 35 0 45 0 Day since 1st Sept. Q m³ /s VHM 205 S O N D J F M A M J J A l l l l l l l l l l l l l l l l l l l l l l l l l l 0 100 200 300 10 0 15 0 20 0 25 0 Day since 1st Sept. Q m³ /s VHM 206 S O N D J F M A M J J A l l l l l l l l l l l l l l l l 0 100 200 300 15 0 25 0 35 0 Day since 1st Sept. Q m³ /s VHM 221 S O N D J F /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 34. Bárðarbunga 2015 - March, April, May

  by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. 12 March 2015 - from the Scientific Advisory Board Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now /earthquakes-and-volcanism/articles/nr/3122

• 35. Bárðarbunga 2015 - March, April, May

  by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. 12 March 2015 - from the Scientific Advisory Board Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now /earthquakes-and-volcanism/articles/nr/3122/

• 36. Bardarbunga-2015_MarchAprMay-events

  monitoring so that warnings may be issued if necessary. Vatnajökull National Park will issue locations of viewing areas. Information on evacuation routes will be issued by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 37. CES_D2.4_solar_CMIP3

  less than 10 MJ m−2. This also holds for autumn, apart from southern Scandinavia where insolation increases by 10-20 MJ m−2. The largest changes occur in spring and summer, with the maximum decreases (increases) of the order of 40 MJ m−2 taking place in north- ern Lapland in spring (southern central Sweden in summer). Note also the substantial decrease in Greenland in summer, 40-60 MJ m−2 /media/ces/CES_D2.4_solar_CMIP3.pdf

• 38. Kok_JGEC658_2009

  after 20–30 iterations, although total stabilisation can take more than 100 iterations. Fig. 2 shows two directed graphs of the Fuzzy Cognitive Map and the development of the values of state vector A for the first 30 iterations. The right-hand side graph has one additional relationship e23 = 0.5. 2.5. Interpretation of Fuzzy Cognitive Maps All input and output of a Fuzzy Cognitive Map is semi /media/loftslag/Kok_JGEC658_2009.pdf

• 39. 2010_003rs

  ........................................................ 19 2.3.2 Changing the maximum number of events in a group ................................. 20 2.3.3 Rearrange order of input .............................................................................. 22 2.3.4 Relocate only the best events ....................................................................... 22 2.3.5 Other tests /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 40. VI_2015_006

  %) Ice-free ocean & Overcast 186 (20%) 22 (12%) 32 (17%) 40 (22%) 92 (49%) 41 whether this also holds for monthly averages. Based on data from an ongoing IMO reanalysis project, this will be the subject of future analyses. References Brousseau, P., Berre, L., Bouttier, F., & Desroziers, G. (2011). Background-error covariances for a convective-scale data-assimilation system: AROME – France 3D-Var /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf