81 results were found for J 소액결제현금화 【TKTAKA༝COM】 티켓타카 K 소액결제현금화 전문 포탈 빠르고론📦disforest/.

Results:

• 1. Climate and Modeling Scenarios

  Elíasson, J., Rögnvaldsson, Ó. & Jónsson, T. (2009). Extracting statistical parameters of extreme precipitation from a NWP model. Hydrol. Earth Syst. Sci., 13, 2233-2240, November 2009. Jylhä, K., Tuomenvirta, H., Ruosteenoja, K., Niemi-Hugaerts, H., Keisu, K. & Karhu, J.A. (2010). Observed and projected future shifts of climatic zones in Europe, and their use to visualize climate change /ces/publications/nr/1680

• 2. 2005EO260001

  up to ~13 km height. BY K. S. VOGFJÖRD, S. S. JAKOBSDÓTTIR, G. B. GUDMUNDSSON, M. J. ROBERTS, K. ÁGÚSTSSON, T. ARASON, H. GEIRSSON, S. KARLSDÓTTIR, S. HJALTADÓTTIR, U. ÓLAFSDÓTTIR, B. THORBJARNARDÓTTIR, T. SKAFTADÓTTIR, E. STURKELL, E. B. JÓNASDÓTTIR, G. HAFSTEINSSON, H. SVEINBJÖRNSSON, R. STEFÁNSSON, AND T. V. JÓNSSON Research, 2005), which are complemented by three continuous GPS stations /media/jar/myndsafn/2005EO260001.pdf

• 3. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 4. Statistical Analysis

  of Hydrology 375: 363-372 (doi:10.1016/j.jhydrol.2009.06.032). Tietäväinen, H. Tuomenvirta, H. & Venäläinen, A. (2009). Annual and seasonal mean temperatures in Finland during the last 160 years based on gridded temperature data. Int. J. Climatol. 29. (in print). Venäläinen, A., Jylhä, K., Kilpeläinen, T., Saku, S., Tuomenvirta, H, Vajda, A. & Ruosteenoja, K. Recurrence of heavy precipitation, dry spells /ces/publications/nr/1943

• 5. VI_2015_009

  Rist, S. (1990). Vatns er þörf. Bókaútgáfa Menningarsjóðs. 248 pp. (In Icelandic). Zaman, M.A., Rahman, A. & Haddad, K. (2012). Regional flood frequency analysis in arid regions. A case study for Australia. J. Hydrol., 475, 74-83. 25 Appendix I - Identification of homogeneous groups of catch- ments obtained with the ROI technique and associated growth curves −2 0 2 4 6 0 1 2 3 4 −ln(−ln(1−1/T)) q(T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 6. 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

• 7. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 8. Paper-Olafur-Rognvaldsson_92

  and hydrologic models at regional scale. Mon. Wea. Rev., 128(6), 1681–1706. Grell, G. A., Dudhia J. and Stauffer D. R. 1995. A description of the fifth- generation Penn State/NCAR Mesoscale Model (MM5). NCAR Tech. Note NCAR/TN-398+STR, 138 pp. Jasper, K., Gurtz J. and Lang H. 2002. Advanced flood forecasting in Alpine watersheds by coupling meteorological observations and forecasts with a dis- tributed /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 9. VI_2015_005

  the two reanalyses exist primarily over Green- land, where the amplitude of the seasonal cycle in ERA-Interim is reduced, with up to 5 K higher temperatures than ERA-40 in winter, and up to 5 K lower temperatures in summer (not shown). Elsewhere, differences are small and unsystematic. As described by Simmons et al. (2006) and Berrisford et al. (2009), compared with ERA-40, sev- eral improvements /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 10. Protective measures

  to avalances: An overview of the need for avalanche protection measures in Iceland (IMO Rep. 96004, 1996, authors T. Jóhannesson, K. Lied, S. Margreth and F. Sandersen) [summary of IMO publication 96003/96004] (html) Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Int. Rep. 99013, 1999, authors T. Jóhannesson and S. Margreth) (pdf 0.1 Mb) Addendum /avalanches/imo/protective/