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82 results were found for R 소액결제현금화 『TKTAKA1 COM』 티켓타카 S 소액결제현금화 전문 포탈 유가증권📹epigraphy/.


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  • 11. Group-1_Scenarios-for-AWM

    i on c a p ac i t y A r ea of r e s i d en c e (Flood p r one /non p r one a r eas) Un c e r t a n t i e s H i g h wi l l i n g n e s s t o p a y L o w wi l l i n g nes to pay D i k e s H i gh t a x a t i on - E arly w arn i n g s y s t e m s - Sof t s t r uct u r a l m e as u r e s -Community training L o w taxation Risk P e r c e p t i o n B e n e f i /media/loftslag/Group-1_Scenarios-for-AWM.pdf
  • 12. Alam_Ashraful_CES_2010

    FOREST BIOMASS FOR ENERGY PRODUCTION – POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki School of Forest Sciences, University of Eastern Finland, Joensuu F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on Oslo, Norway 2 June, 2010 Contents • Forestry in Finland • Challenges • Objectives /media/ces/Alam_Ashraful_CES_2010.pdf
  • 13. IPPC-2007-ar4_syr

    TS.1b, TS.2b} Global anthropogenic GHG emissions F-gases CO2 from fossil fuel use and other sources CH4 from agriculture, waste and energy CO2 from deforestation, decay and peat N2O from agriculture and others GtC O 2-eq / y r 28.7 35.6 39.4 44.7 49.0 The largest growth in GHG emissions between 1970 and 2004 has come from energy supply, transport and industry, while resi- dential and commercial /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 14. VI_2015_009

    ll l ll l l l l l l l l l l l H1−ROI: 0.848 H1−ROI+vhm167: 1.69 Figure I.3. As Fig. I.I but for vhm238 (top-left), vhm144 (top-right), vhm145 (bottom-left), vhm167 (bottom-right). 28 Appendix II - Index flood estimation at gauged sites treated as ungauged. l l l l l l l l l l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0)(A)(θ1) Rel. RMSE= 0.87 NS= 0.8 MAE= 83 l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 15. GA_2009_91A_4_Andreassen

    - elled using precipitation data southwest of the gla- cier. Results from the model compared well with re- ported mass balance values for the period 1949– 2006, obtained correlations (r) for bw and bs varied between 0.83 and 0.87 depending on model set up. Reconstruction of the mass balance series for the period 1924/1925–1948/1949 suggested a cumula- tive mass deficit of c. 30 m w.e. mainly due /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 16. 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
  • 17. ces_SA_group_flyer_new

    series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf
  • 18. AnneFleig_May2010_CES

    E l b e i n D r e s d e n , A p r i l 2 0 0 7 CES conference, Oslo, Norway, 31 May - 2 June 2010 Typical features • develop slowly, • become severe when they cover a large region and persist for an extended period. E l b e i n D r e s d e n , A p r i l 2 0 0 7 ( s p i e g e l . d e ) Anne K. Fleig et al. “Regional hydrological droughts and weather types in north /media/ces/AnneFleig_May2010_CES.pdf
  • 19. Sigurður Th. Rögnvaldsson

    21.06.1999. Sigurður Th. Rögnvaldsson, Reynir Böðvarsson, R. Slunga og Steinunn S. Jakobsdóttir 1997. The transfer function of the SIL seismic data acquisition system. Rit Veðurstofu Íslands VÍ-R97001-JA01. Sigurður Th. Rögnvaldsson, Ágúst Guðmundsson og R. Slunga 1998. Seismotectonic analysis of the Tjörnes Fracture Zone, an active transform fault in north Iceland. J. Geophys. Res. 103, 30117 30129 /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/
  • 20. Sigurður Th. Rögnvaldsson

    21.06.1999. Sigurður Th. Rögnvaldsson, Reynir Böðvarsson, R. Slunga og Steinunn S. Jakobsdóttir 1997. The transfer function of the SIL seismic data acquisition system. Rit Veðurstofu Íslands VÍ-R97001-JA01. Sigurður Th. Rögnvaldsson, Ágúst Guðmundsson og R. Slunga 1998. Seismotectonic analysis of the Tjörnes Fracture Zone, an active transform fault in north Iceland. J. Geophys. Res. 103, 30117 30129 /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

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