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82 results were found for R 소액결제현금화 『TKTAKA1 COM』 티켓타카 S 소액결제현금화 전문 포탈 유가증권📹epigraphy/.


Results:

  • 31. 2013_001_Nawri_et_al

    is absolute air temperature (in degrees Kelvin), h is local terrain elevation above mean sea level (as a function of the horizontal coordinates), z is height above ground, g = 9.81 m s 2 is the gravitational constant, and R = 287 J K 1 kg 1 is the specific gas constant of dry air. Nawri et al. (2012a) showed that seasonal averages of surface air temperature over Iceland decrease linearly /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 32. Hydropower - Glacier, Snow and Ice

    by remote sensing. Polar Research 2011, 7282, doi: 10.3402/polar.v30i0.7282 Guðmundsson, S., Björnsson, H., Jóhannesson, T., Aðalgeirsdóttir, G., Pálsson, F. & Sigurðsson, O. (2009). Similarities and differences in the response of two ice caps in Iceland to climate warming. Hydrology Research. 40(5), 495-502. Schuler, T. V., Crochet P., Hock R., Jackson M., Barstad I. & Jóhannesson, T. (2008 /ces/publications/nr/1940
  • 33. vanRoosmalen_etal-2009-WRR_2007WR006760

    The hydraulic conduc- tivity of the sand formations is generally high, of the order of 104–103 m/s [Harrar et al., 2003; Sonnenborg et al., 2003]. In general, groundwater flows from east to west. At the water divide to the east the hydraulic head level is about 75 masl, decreasing to sea level at the west coast. The average head gradient is 0.001. The seasonal variation in head values is generally less /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 34. VI_2015_005

    hPa in winter, and up to 5 hPa in summer, with small and unsystematic differences elsewhere (not shown). As shown in Figure 2, surface (10-m) wind speed in ERA-Interim is generally higher than in ERA-40. In coastal regions, over Iceland, and across southern Greenland, differences are up to 3 m s 1 in winter. Differences over the ocean are relatively small. Over land, differences are not 9 Figure /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 35. VI2010-006_web

  • 36. TietavainenHanna_CES_2010

    the observed data sets are smaller in SW than in NE • MMM overestimates precipitation, but is closer to observations in SW than NE barb2right Better observational coverage in SW SW NE p r e c i p i t a t i o n s u m ( m m ) CES Conference, Oslo 31.5.-2.6.2010 SWNE • Precipitation trends (mm / 10 yr) in 1961-2000 according to observations and model simulations (MMM) • Including the range /media/ces/TietavainenHanna_CES_2010.pdf
  • 37. aerodrome_summaries_20140603

    M (171FT ) FRE Q UENCIE S (PE R CENT ) O F OCCU R RENC E O F CONCURREN T WIN D DIRECTIO N (I N 30 0 SEC T ORS ) AN D SPEE D (I N KN O TS ) WITHI N SPECIFIE D RANGE S ANN U A L WIN D WIN D SPEE D (KT) ) DIRECTIO N CAL M 1– 5 6–1 0 11–1 5 16–2 0 21–2 5 26–3 0 31–3 5 36–4 0 41–4 5 46–5 0 >5 0 T O T A L V ARIABL E 0 0 0 0 0 0 0 0 0 0 0 0 0 35-36-0 1 3 2 3 3 2 1 1 0 0 0 0 0 14 02-03-0 4 0 2 4 4 3 1 0 0 /media/vedur/aerodrome_summaries_20140603.pdf
  • 38. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    h stat us an d goal s Locat io n — u n ce rta in tie s re la te d to So urc e o fun certaint y Natur e (1)/typ e(2 )o f u n ce rta in ty Co mment s R hin e at (su b-) catch m en tleve l W at er re so u rc es issu es Id en tif ica tio n an d pr io rit y settin g o fu rge nt wat er re so u rc es pr ob le m s; co n fli ct in g in te re sts amon g sector s an d stakeh older s M ul tip le fra m es (so /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 39. Refsgaard_etal-2007-Uncertainty-EMS

    on the quantity at hand (strengths and weaknesses in Box 1. The error propagation equation The error propagation equations for the most common operators are (s is the standard deviation): Addition and Subtraction: z ¼ x þ yþ/ or z ¼ x  y/ sz ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi s2x  þ  s2y  þ/ r Multiplication by an exact number: z /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 40. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

    ORIGINAL ARTICLE The role of uncertainty in climate change adaptation strategies—A Danish water management example J. C. Refsgaard & K. Arnbjerg-Nielsen & M. Drews & K. Halsnæs & E. Jeppesen & H. Madsen & A. Markandya & J. E. Olesen & J. R. Porter & J. H. Christensen Received: 10 November 2011 /Accepted: 4 February 2012 # The Author(s) 2012. This article is published with open access /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

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