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


  • 31. Staff members

    Staff members Þorsteinn V. Jónsson Job title: Meteorologist Email /about-imo/employees/persona/85/fyrirtaeki/2
  • 32. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    em ic 2: St at ist ic al / qu al ita tiv e/r ec og ni se d igno ranc e O fte n im po rta nt Pa rti ci pa to ry pr oc es se s to re du ce u n ce rta in ty :I nt eg ra te d ba sin m o de lf or th e R hine :DS S fo rsup portin g decisio n ma kin g o n e.g .floodin g an d poll utio n (w ate r,e co n o m ic s an d u n ce rta in ty ). cli m at e ch an ge an d v ar iab ili ty so cio ec o no m ic de v elo /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 33. Hydropower - Glacier, Snow and Ice

    Publications and presentations Hydropower - Glacier, Snow and Ice International w/peer-review Aðalgeirsdóttir, G /ces/publications/nr/1940
  • 34. 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
  • 35. Dyrrdal_Anita_CES_2010

    Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf
  • 36. Linnet_Ulfar_CES_2010

    2015, 2025, 2035 and 2050 North (Blanda) East (Karahnjukar) South (Thorisvatn) Change in average inflow to the main storage reservoirs Watershed A v e r a g e i n f l o w [ m 3 / s ] 0 2 0 4 0 6 0 8 0 1 0 0 1 2 0 Last 50 years Last 20 years Last 15 years Last 10 years Last 5 years Temperature corrected Transformation of climate measurements •Change in temperature • 0.75 °C/100y 1950-1975 • 1.55 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 37. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    & 4 Y u a n g Z h e n g D e n m a r k F o r e s t r y & L a n d s c a p e 2 1 0 A t h a n a s i o s V o t s i s F i n l a n d U r b a n & r e g i o n a l p l a n n i n g 3 3 2 E i v i n d J u n k e r N o r w a y L a w 4 3 3 M i c h a e l L a i h o F i n l a n d E u r o p e a n s t u d i e s 5 2 0 H e c to r G u i n e a B a r r i e n to s S w e d e n N a t u r a l r e s o u /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 38. 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
  • 39. VI_2013_006

    and longitude °W (Meðalstaðsetning / Breidd Lengd), median location, latitude °N and longitude °W (Miðgildi / Breidd Lengd), radius of a circle around the median location which encloses half of the observed lightning (Helm fjarl), and distance (km) and direction (N=North, A=East, S=South, V=West) from a named reference place (Viðmið). Currently, no wind correction is automatically included. Data /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
  • 40. 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

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