78 results were found for P 출장마사지☏ㄲr톡 gttg5☏ૉ간석오거리출장모텔㻿간석오거리출장샵䤿간석오거리출장서비스䟶간석오거리출장숙소👨🏽‍🚒reimburse/.

Results:

• 41. 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

• 42. VI_2009_013

  ). The brittle-plastic transition and depth of seismic faulting, Geol. Rundsch., 77, 319–328. Scholz, C. H. (2002). The Mechanics of Earthquakes and Faulting, 2nd ed., Cambridge Univ., Cambridge. Sibson, R. H. (1984). Roughness at the Base of the Seismogenic Zone: Contributing Factors.J. Geophys. Res., 89, B7, 5791–5799. Sigmundsson, F., P. Einarsson, R. Bilham, and E. Sturkell (1995). Rift-transform /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 43. 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

• 44. 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

• 45. Lettenmaier_Dennis_CES_2010pdf

  12 1 month 12 Columbia River Basin Water Resource Sensitivity to PCM Climate Change Scenarios 0% 20% 40% 60% 80% 100% 120% Portland- Vancouver Spring Flood Control Reliability Portland- Vancouver Winter Flood Control Reliability Autumn Firm Power Reliability (November) % of Control Hydropower Revenues McNary Instream Target Reliability (April- August) Middle Snake Agricultural /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 46. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  tg ui da n ce fo rt ra ns bo un da ry w at er s, pr ep ar ed an d P. van der Keur et al. (floo dmanag ement )an d wat er qualit y ag re ed u po n in co m m o n u n de rs ta nd in g, creat ed th e bas is fo rth e formul atio n o f joi nt m ea su re s (Fr ijte rs an d Le en tv aa r 200 3) Mo del s (na tural ,te chnica l an d so ci al sy ste m s): Uncert aint y ha s to be incorp orated : 1: Ep ist /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 47. Kok_and_Veldkamp_editorial_ES-2011-4160

  ? Methodological reflections on scalar structuration. Progress in Human Geography 25:591-614. Bryan, B. A., N. D. Crossman, D. King, W. S. Meyer. 2011. Landscape futures analysis: assessing the impacts of environmental targets under alternative spatial policy options and future scenarios. Environmental Modelling and Software 26(1):83-91. Buizer, M., B. Arts, and K. Kok. 2011. Governance, scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 48. Cradden_Lucy_CES_2010

  ? • Based on thermodynamic and heat transfer models accounting for: Wire resistance Solar heating Radiative cooling Convective cooling June 2010 7 How are ratings determined? • UK network standards assume seasonal average temperatures and worst-case wind conditions, i.e. low wind speeds Summer → 20˚C; Spring/Autumn → 9˚C; Winter → 2˚C • Real-time monitoring (‘dynamic rating’) is not commonly /media/ces/Cradden_Lucy_CES_2010.pdf

• 49. 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

• 50. Sigurður Th. Rögnvaldsson

  of the joint use of P wave polarization and travel-time data in tomographic inversion: Crustal velocity structure near the South Iceland Lowland network. Geophys. Res. Lett. 20, 1407-1410. Kristín S. Vogfjörð og Sigurður Th. Rögnvaldsson 1999. Identification and modeling of secondary phases in short-period seismograms from local earthquakes in the South Iceland seismic zone. Óbirt grein. Kristján /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/