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


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  • 21. VI2010-006_web

    490 þar af regn 5 1 3 4 10 27 32 33 32 27 6 4 185 þar af slydda 22 14 13 12 8 1 1 1 6 21 20 16 135 þar af snjór 29 27 27 13 1 0 0 0 1 9 28 32 169 Mest á dag (mm) 31 37 41 28 31 42 20 25 25 39 28 21 42 Fjöldi regndaga 2 2 2 2 5 10 12 12 11 9 3 2 75 Fjöldi snjó/slyddud. 14 12 15 10 4 1 0 0 2 8 13 16 96 Fjöldi úrkomudaga 17 14 16 12 10 11 12 13 14 17 16 18 171 Meðalhiti (◦C) −2.2 −1.5 −1.3 1.6 5.5 9.1 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
  • 22. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    pm en t. Co ntex t(natura l,techni ca l an d so ci al sy ste m s): tra ns bo un da ry iss ue s w ith man y di ffe ren tspa tia lsc ales . So ci o ec o n o m ic an d cl im at e chang e ar e imp ortan t 1:Ont ologica l2:Sce nari o O fte n domina nt D ominant :Compl ex Int egrate d Sy ste m A na ly sis (C ISA ): in te gr at ed m o de lli ng an d as se ss m en tf or ex am in at io n o f co m pl ex re /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 23. 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
  • 24. 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
  • 25. Sea ice in August 2009

    in the period 6th to the 22nd, eight from ships and one from land. The icebergs were closest to land at 66°28,81'N og 21°23,86'V and close to Selsker (66°07,5N og 21°31'V). No seaice was in the Greenland Strait in August and northeasterly winds prevailed in the area /sea-ice/monthly/2009/nr/2330
  • 26. ces-glacier-scaling-memo2009-01

    respresenting the relationship (5) betweeen ice volume and ice- covered area for Icelandic ice caps (v = csg with c = 0:048 and g= 1:23). Over the first 50–100 years, the simulated decreasing ice volume becomes progressively lower than would correspond to the ice-covered area at the same point in time. The rapid glacier retreat thus results in an ice volume that is 20% less than predicted /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 27. VI_2017_009

    we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf
  • 28. Hydropower - Glacier, Snow and Ice

    glacier-scaling-hydrological model. 88-89. Machguth, H., & Ahlstrøm, A. (2010). Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties. p. 42-43. Melvold, K. & Laumann, T. (2010). A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES). 90-91. Radic, V /ces/publications/nr/1940
  • 29. Staff members

    Staff members Þorsteinn V. Jónsson Job title: Meteorologist Email /about-imo/employees/persona/85/fyrirtaeki/2
  • 30. Lawrence_Deborah_CES_2010

    100 15 17 19 21 23 25 Mean annual peak runoff (mm/day) P e r c e n t a g e b e l o w g i v e n v a l u e g39g72g79g87g68g3g70g75g68g81g74g72g3 g40g80g83g76g85g76g70g68g79g3g68g71g77g88g86g87g80g72g81g87 Percentage change in 200-year flood Uncertainty – Relative magnitude of sampled s urces N = 115 GCM/RCM = 50 EA/DC = 38 HBV = 27 • Differences in GCM/RCM tend to be more significant in inland /media/ces/Lawrence_Deborah_CES_2010.pdf

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