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13 results were found for 미국지수거래《www༝88m༝kr》www༝88m༝kr 케이티비스팩1호 중앙백신⊙일진머티리얼즈㏱이연제약 ー褖 inconsistent.


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  • 1. CES_D2_2_poster_3x3

    CMIP3 Multimodel Dataset: A New Era in Climate Change Research. Bulletin of the Americal Meteorological Society, 88, 1383-1394. Naki enovi , N. and R. Swart (Eds.) 2000: Emission Scenarios. A Special Report of Working Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press, 599 pp. Räisänen, J. and L. Ruokolainen 2006: Probabilistic forecasts of near-term climate /media/ces/CES_D2_2_poster_3x3.pdf
  • 2. Protective measures

    experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html) Stálgrindur eða snjóflóðanet? Val á tegund /avalanches/imo/protective/
  • 3. 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
  • 4. 2010_005_

    for Iceland were made. The CE project used an ensemble of six GCMs and RCMs from the PRUDENCE project for four different emissions scenarios (B1, B2, A2, and A1FI) developed by the Intergovernmental Panel on Climate Change (IPCC). The GCMs used by the CE project showed more warming during winter than summer. During winter, the median projected warming from 1961–90 to 2070–99 ranged from 3–6 K, and from 2 /media/ces/2010_005_.pdf
  • 5. VI_2009_012

    Distance corrected PGV. ......................... 14  Figure 3. Corrected magnitudes, Mw(v) plotted against log distance.. .................................. 17  Figure 4. Magnitude estimates as a function of Ci. ................................................................ 18  Figure 5. Observed/predicted PGV residuals for each station. .............................................. 20  Figure 6 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 6. Perrels-CBA

    / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf
  • 7. VED_AnnualReport-2013_screen

    (). The circulation of Icelandic waters-a modelling study. Ocean Science , –. Nygaard, B. E. K., Hálfdán Ágústsson & K. Somfalvi-Toth (). Modeling wet snow ac- cretion on power lines: improvements to previ- ous methods using  years of observations. Journal of Applied Meteorology and Climatology (), –. Philippe Crochet (). Sensitivity of Icelandic river basins to recent /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
  • 8. Kok_et_al._TFSC_published_2011

    of EC-funded projects. This paper reports on activities that took place within the SCENES project (www.environment. /syke/scenes), which set out to undertake a multi-dimensional multi-scale scenario process, with a strong foundation in science and broad participation of stakeholders. This should provide new ideas about managing the future of water in Europe. Scenarios were developed at three scales /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
  • 9. VI_2020_005

    (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 10. VI_arsskyrsla2020

    og dreifingu gjósku í eldgosum. Í kjölfar Eyjaallajökulsgossins 2010 bættist önnur við á Austurlandi og síðan tvær færanlegar, sérstaklega til þess að vakta eldgosavá. Mynda- safn Veðurstofu Íslands. 20 ÁRSSKÝRSLA 2019 Brúarfoss. Ljósmynd: Einar Guðmann. 21 „TÍMI OG BREYTILEIKI Í VATNAFRÆÐI“ Í tilefni af 50 ára afmæli Vatnamælinga 1997 „Í dag stöndum við andspænis þeirri staðreynd, að /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

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