84 results were found for B 신용카드현금화 〔TKTAKA1-CՕM〕 티켓타카 C 신용카드현금화 전문 포탈 ‎고객센터🇮🇸grotesquely/.

Results:

• 51. Climate and Modeling Scenarios

  Clausen, N.-E., Pryor, S. C., Guo Larsén, X., Hyvönen, R., Venäläinen, A., Suvilampi, E., Kjellström, E., Barthelmie, R. (2009). Are we facing increasing extreme winds in the future? EWEC 2009 Marseille session DT2A, 19 March 2009. Engen-Skaugen,T & Førland, E.J. (2010). Future change in return values and extreme precipitation at selected catchments in Norway, met.no Report 20/2010 (draft). Engen /ces/publications/nr/1680

• 52. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  Identification of Major Sources of Uncertainty in Current IWRM Practice. Illustrated for the Rhine Basin P. van der Keur & H. J. Henriksen & J. C. Refsgaard & M. Brugnach & C. Pahl-Wostl & A. Dewulf & H. Buiteveld Received: 13 December 2006 / Accepted: 10 January 2008 # Springer Science + Business Media B.V. 2008 Abstract Integrated Water Resources Management (IWRM) can be viewed as a complex /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 53. 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

• 54. Water_resources_man_Veijalainen_etal

  0 50 0 J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D 2010–39(a) 0 10 0 20 0 30 0 40 0 50 0 2040–69(b) Lake Pielinen 0 10 0 20 0 30 0 40 0 50 0 2070–99(c) 0 1 0 3 0 5 0 7 0 2010–39(d) 0 1 0 3 0 5 0 7 0 2040–69(e) Lake Syväri 0 1 0 /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 55. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  treduced ,o r resolved ,i n orde rt o preven tstallin g o fth e decision-makin g process .Inclusive :n o stallin g becaus e o fthi s spec ifi c conflict ,exclusiv e othe rconflict s b Whe n researc h result sar e presented ,i ti spossibl e (in general )t o hav e an ope n discussio n an d provid e critica lfeedbac k o n th e conceptua lframewor k, researc h methods ,results ,an d conclusion s(ofte nb y /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

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

  derived from: (a) SPOT 5 high-resolution stereoscopic images from 5 October 2004; (b) SPOT 5 HRS from 14 August; (c) Electromagnetic Institute Synthetic Aperture Radar Sensor (EMISAR) images from 12 August 1998; and (d) aerial photographs from 1979 (Torfajo¨kull), 1980 (Tindfjallajo¨kull) and 1984 (Eyjafjallajo¨kull). Gaps in (a) and (b) allocate uncorrelated parts of the SPOT 5 HRS image pairs /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 57. Journal_of_Hydrology_Veijalainen_etal

  in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 58. Kok_1-scenarios-lecture-1

  scale: The Hierarchy Theory • Emerged as part of a movement toward a general science of complexity • Rooted in various other disciplines but operationalised by ecologists in the 1970s and 1980s • Key references: Allen, T. F. H. and T. B. Starr. 1982. Hierarchy: perspectives for ecological complexity. University Chicago Press. Allen T. F. H. and T. Hoekstra. 1992. Toward a unified ecology /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 59. ces-oslo2010_proceedings

  ) for different periods in the past. By combining observations from the NVE and met.no networks, we are able to obtain results from the entire elevation profile. 11 Figure 1: Correlation coefficient (R) between time series of: a) number of snow days and winter temperature, b) number of snow days and winter precipitation, c) annual maximum snow depth and winter temperature, and d) annual maximum /media/ces/ces-oslo2010_proceedings.pdf

• 60. Eyjafjallajökull eruption 2010 - the role of IMO

  in April-May 2010, IMO monitored the volcanic activity through various geophysical sensors (seismic, strain, GPS), river runoff from the glacier and the behaviour of the volcanic eruption cloud (see slide show). The main tool for monitoring the volcanic cloud was a C-band weather radar located at Keflavik international airport, approximately 150 km west of the volcano (see map below). Plume height /earthquakes-and-volcanism/articles/nr/2072