78 results were found for P 출장안마〔ㄲr톡 GTTG5〕䬶개화예약금없는출장翧개화오전출장俾개화오후출장Ṏ개화외국녀출장🇬🇳reflexive/.

Results:

• 41. norsem_buhcheva

  located events to invert for a new 1D minimum velocity model for both P- and S-waves using VELEST. A depth region of a lower vpvs ratio down to 20 km depth is revealed. We perform relocation of the whole dataset using the new velocity model and the double-difference relocation technique. We look into details of the depth distribution of the events and how the relocation procedure affects /media/norsem/norsem_buhcheva.pdf

• 42. norsem_schmidt

  will occasionally have to deal with spurious events. At SNSN we are therefore investigating the feasibility to construct an event verifier. The basic idea is to emulate the decision made by a seismologist viewing a section of recorded traces, sorted by epicentral distance, and expecting to see direct P-phase arrivals on most traces out to the most distant phase pick. Here we will report /media/norsem/norsem_schmidt.pdf

• 43. VI_2009_013

  ...................................... 18  Figure 7. Temporal/spatial evolution of seismicity between 1996 and 2007. .................. 19  Figure 8. Temporal/spatial evolution during the latter intrusion swarm and until 2006. . 19  Figure 9. Mechanisms in selected depth intervals for the three main swarms. ................ 21  Figure 10. Distribution of P- and T-axis for events /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 44. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 45. Climate and Modeling Scenarios

  & Ólafsson, H. (2010). Validation of numerical simulations of precipitation in complex terrain at high temporal resolution. Hydrology Research, 41 (3-4), 164-170. Christensen, J.H., Boberg, F., Christensen, O.B. & Lucas-Picher, P. (2008), On the need for bias correction of regional climate change projections of temperature and precipitation, Geophys. Res. Lett., 35, L20709, doi:10.1029/2008GL035694 /ces/publications/nr/1680

• 46. Lettenmaier_Dennis_CES_2010pdf

  Dennis P. Lettenmaier Department of Civil and Environmental Engineering University of Washington Conference on Future Climate and Renewable Energy: Impacts, Risks, and Adaptation Oslo June, 1, 2010 Runoff projections and impacts on water resources Outline of this talk 1) Projected runoff changes over the next century – the global and continental picture 2) Downscaling to the regional /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 47. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  Identification of Major Sources of Uncertainty in Current IWRM Practice. Illustrated for the Rhine Basin P. van der Keur & H. J. Henriksen & J. C. Refsgaard & M. Brugnach & C. Pahl-Wostl & A. Dewulf & H. Buiteveld Received: 13 December 2006 / Accepted: 10 January 2008 # Springer Science + Business Media B.V. 2008 Abstract Integrated Water Resources Management (IWRM) can be viewed as a complex /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 48. Kok_and_Veldkamp_editorial_ES-2011-4160

  Tengö, D. Timmer, and M. Zurek. 2007. Linking futures across scales: a dialog on multiscale scenarios. Ecology and Society 12(1): 17. [online] URL: http://www.ecolog yandsociety.org/vol12/iss1/art17/. Borgatti, S. P., and P. C. Foster. 2003. The network paradigm in organizational research: a review and typology. Journal of Management 29(6):991-1013. Brenner, N. 2001. The limits to scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 49. Cradden_Lucy_CES_2010

  Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf

• 50. Dyrrdal_Anita_CES_2010

  Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute met.no Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf