69 results were found for V 신용카드현금화 〔TKTAKA1-CՕM〕 티켓타카 W 신용카드현금화 전문 포탈 핸드티켓⛳denunciator/.

Results:

• 41. Benestad_Rasmus_CES_2010

  wind Obs=ERAINT (reanalysis) righttoleftmark Storm statistics Domain: 12°W-38°E/48-66°N (Same as RCM) Historical reanalysis ERAINT Little trend! Historical analysis: N CCI on small domain: restricted RCM domain Domain: 80°W-40°E/20- 75°N Different story! Geographical distribution? Storm statistics: Whole North Atlantic Homogeneous? Historical analysis: |v| Southern Norway SLP 'triangulation /media/ces/Benestad_Rasmus_CES_2010.pdf

• 42. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  was used as a reference map for co-registration and correction of the vertical offset of the other DEMs. The average specific mass balance was estimated from the mean elevation difference between glaciated areas of the DEMs. The glacier mass balance declined significantly between the two periods: from 0.2 to 0.2 m yr1 w. eq. during the earlier period (1980s through 1998) to 1.8 to 1.5 m yr1 w /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 43. Kok_1-scenarios-lecture-1

  : to use or not to use? *O'Neill, R. V., and A. W. King. 1998, Homage to St. Michael; or, why are there so many books on scale?: Pages 3–15 in D. L. Peterson and V. T. Parker (editors). Ecological scale: theory and applications. Columbia University Press, New York. • Robert O’Neill questions the unifying capabilities* • Aspects of the land use system have different scale properties • To use /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 44. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  L. G. (1977). The economics of fisheries management. Baltimore: Johns Hopkins University Press. Berkes, F., Feeny, D., McCay, B. J., & Acheson, J. M. (1989). The benefits of the commons. Nature, 340, 91–93. Blomquist, W. (1992). Dividing the waters: governing groundwater in Southern California. San Francisco: ICS Press. Bromley, D. W., Feeny, D., McKean, M., Peters, P., Gilles, J., Oakerson, R /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 45. VI_2015_009

  all sites was calculated (RMSET ): RMSET (%) = 1 N N i=1 v u u t1 L L l=1 Qi(D;Tl) bQi(D;Tl) Qi(D;Tl) 2 x100 (7) where Qi(D;Tl) is the reference flood quantile at gauged site i and return period Tl , calculated with the GEV distribution fitted to the observed AMF series and bQi(D;Tl) is the estimated flood quantile, calculated with the IFM ( bQi(D;T ) = bµi(D)qR(D;T )). RMSET was ranked /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 46. IPPC-2007-ar4_syr

  and are expressed in watts per square metre (W/m2). 5 Includes only carbon dioxide (CO2 ), methane (CH4), nitrous oxide (N2O), hydrofluorocarbons (HFCs), perfluorocarbons (PFCs) and sulphurhexafluoride(SF6), whose emissions are covered by the UNFCCC. These GHGs are weighted by their 100-year Global Warming Potentials (GWPs), using values consistent with reporting under the UNFCCC. 6 This report /media/loftslag/IPPC-2007-ar4_syr.pdf

• 47. Milly_etal-2008-Stationarity-dead-Science

  A. Dunne, A. V. Vecchia, Nature 438, 347 (2005). 16. J. C. Knox, Quatern. Sci. Rev. 19, 439 (2000). 17. P. C. D. Milly, R. T. Wetherald, K. A. Dunne, T. L. Delworth, Nature 415, 514 (2002). 18. Z. W. Kundzewicz et al., Hydrol. Sci. J. 50, 797 (2005). 19. R. Seager et al., Science 316, 1181 (2007). 20. IPCC, in Climate Change 2007: Mitigation of Climate Change, Contribution of WG3 to AR4, B /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 48. VI_2015_006

  Differences in net shortwave flux due to differences in cloud cover (compare with Figure 5) are especially noticeable on 27 July and 3 August around (local) noon when, off the south and southwest coast, the net flux under clear skies is increased by up to 300 W m 2, compared with neighbouring cloud-covered regions. Although, generally, there was a more extensive cloud cover over the land on 3 August than /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 49. Kok_and_Veldkamp_editorial_ES-2011-4160

  2004. Further towards a taxonomy of agent-based simulation models in environmental management. Mathematics and Computers in Simulation 64(1):25-40. Henle, K., W. Kunin, O. Schweiger, D. S. Schmeller, V. Grobelnik, Y. Matsinos, J. Pantis, L. Penev, S. G. Potts, I. Ring, J. Similä, J. Tzanopoulos, S. van den Hove, M. Baguette, J. Clobert, L. Excoffier, E. Framstad, M. Grodzinska-Jurczak, S. Lengyel, P /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 50. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf