91 results were found for D 정보이용료현금화 『TKTAKA1 COM』 티켓타카 E 정보이용료현금화 전문 포탈 캐시나라🧏🏾dismantle/.

Results:

• 51. 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

• 52. Lorenzoni_Pidgeon_2006

  : PidgeonN@cardiff.ac.uk Climatic Change (2006) 77: 73–95 DOI: 10.1007/s10584-006-9072-z c© Springer 2006 74 I. LORENZONI AND N. F. PIDGEON national policies strongly on fossil fuels. The British Prime Minister encapsulated these tensions when he recently stated that there is “no bigger long-term question facing the global community” than climate change (BBC, 2004), whilst emphasising the need /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 53. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 54. Dyrrdal_Anita_CES_2010

  : Significant at 90% CL Norwegian Meteorological Institute met.no Fokstugu (973 m.a.s.l.) Introduction Data & Methods Results Trends in start and end: Significant at 99% CL /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 55. VI_2020_004

  Figure 53 Impact map for airports in case of an eruption like 1362 at Öræfajökull ................ 82 Figure 54 Impact map for power lines in case of an eruption like 1362 at Öræfajökull ......... 83 Figure 55 5% PM10 probability map for an eruption like 1362 at Öræfajökull. ...................... 84 Figure 56 25% PM10 probability map for an eruption like 1362 at Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 56. 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

• 57. VI_2009_006_tt

  was therefore formed by ice lifting and deformation induced by subglacial water pressures higher than ice overburden pressure. The discharge data and the derived size of the subglacial flood path, as indicated by the volume of water stored subglacially, indicates a development towards more efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the iii range 80–90 m3 s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 58. Mid-Latitudes-Agenda1_nov2013EH

  ? – D Wheeler Simulations of the impact of Arctic sea ice on the atmospheric circulation: the need for coupled models – D Smith Greenland Blocking and North Atlantic Oscillation changes – E Hanna / J Overland Group Discussion 12:45 – 14:00 Lunch (after which we move into the matsalur - lunch hall) 14:00 – 15:40 14:00 – 14:20 14:20 – 14:40 14:40 – 15:00 15:00 – 15:20 15:20 – 15:40 /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 59. Kurpniece_Liga_CES_2010

  distribution of runoff under present and future conditions, Plavinas HPP 0.0 200.0 400.0 600.0 800.0 1000.0 1200.0 1400.0 1600.0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec D i s c h a r g e m 3 / s Observed 1961-90 SMHI-RCA3-BMC A1B 2021-50 DMI-HIRLAM-ECHAM5 A1B 2021-50 MetNo-HIRLAM-HadCM3 A1B 2021-50 Observed and modeled runoff , Plavinas 0.00 200.00 400.00 600.00 800.00 1000.00 1200.00 /media/ces/Kurpniece_Liga_CES_2010.pdf

• 60. glacier_mass_balance_poster

  750-1170 AAR of the warm year of 2004 - digitized using the October 2004 SPOT 5 HRS images Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull AAR (%) 20-25 <5 0 Method References Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images. Geophys. Res. Lett., 31, L17401, doi:10.1029 /media/ces/glacier_mass_balance_poster.pdf