91 results were found for y 해킹DB↑《ㅌㄹSein07’チ해킹DB 해킹디비팝니다 해킹디비 해킹디비팝니다.

Results:

• 61. Bárðarbunga 2014 - December events

  moment release is observed before the onset of the fissure eruption (red bar), i.e. while the dyke was growing, and the moment release in the dyke is now 10,000 times less than it was before the eruption (logaritmic scale on y-axis). For the caldera (lower panels), things are a bit more complicated, although a clear trend of decreasing activity is found there as well. Most moment is released during /earthquakes-and-volcanism/articles/nr/3055/

• 62. Bardarbunga-2014_December-events

  has been done (see link). The situation is quite evident for the dyke intrusion (upper panels): The highest moment release is observed before the onset of the fissure eruption (red bar), i.e. while the dyke was growing, and the moment release in the dyke is now 10,000 times less than it was before the eruption (logaritmic scale on y-axis). For the caldera (lower panels), things are a bit more /media/jar/Bardarbunga-2014_December-events.pdf

• 63. ces_geus_paakitsoq_full_report

  of Geophysical Research, 108(D3), 4124, doi:10.1029/2002JD002287. IPCC (2001), Climate change 2001: the scientific basis. Contribution of working group I to the third assessment report of the intergovernmental panel on climate change. (eds. Houghton, J. T. , Y. Ding, D. J. Griggs, M. Noguer, P. J. van der Linden, X. Dai, K. Maskell and C. A. Johnson), Cambridge University Press, Cambridge, UK /media/ces/ces_geus_paakitsoq_full_report.pdf

• 64. Kok_and_Veldkamp_editorial_ES-2011-4160

  2004. Further towards a taxonomy of agent-based simulation models in environmental management. Mathematics and Computers in Simulation 64(1):25-40. Henle, K., W. Kunin, O. Schweiger, D. S. Schmeller, V. Grobelnik, Y. Matsinos, J. Pantis, L. Penev, S. G. Potts, I. Ring, J. Similä, J. Tzanopoulos, S. van den Hove, M. Baguette, J. Clobert, L. Excoffier, E. Framstad, M. Grodzinska-Jurczak, S. Lengyel, P /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 65. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 66. VI_2014_006

  Seasonal effects were taken into account by defining a moving temporal window of K days centered on the target day, for the selection of weather analogues, so that in an archive made of Y years, each target day was at most associated to Y x (2K+1) potential analogues. By doing so, it is hoped that candidate situations will present similar characteristics in terms of solar energy, surface fluxes /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 67. Adalgeirsdottir-etal-tc-5-961-2011

  /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 68. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 69. Kok_et_al._TFSC_published_2011

  explorator y scenarios .Arrow s indicat e th e overal ldirectio n o fchang e durin g th e scenari o perio d acros s Europe ; regiona ldifference s an d short-ter m variabilit y ar e no t represente d here . 843K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy 3.4.3. Key obstacles and opportunities In total 71 obstacles and opportunities were identied /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 70. Journal_of_Hydrology_Veijalainen_etal

  24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf