49 results were found for Z 리플거래「wwwͺbybͺpw」 리플매매 리플투자ิ리플리딩㊌케이엘넷 kCi.

Results:

• 41. Water_resources_man_Veijalainen_etal

  Based on a report by Verta et al. (2007) 92. 5 93. 0 93. 5 94. 0 94. 5 95. 0 M A MJ F J J A S O N D Mean 19702000 Min and max 1970–2000, natural rating curve Target water level zone 1 Target water level zone 2 Q=+20% Q=+10% Q= 0% Q=15% Q=30% 92.90 m snow target 1 92.70 m snow target 2 Water level (m ) Month the regulation limits Lake Syväri has target water level zones, which are not legally /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 42. Eriksson_Garvill_Nordlund_2006

  (see e.g. Steg, 2003). In studies from several countries, push measures are perceived as less acceptable compared to pull measures (e.g. Ho¨lzer, 2003; Rienstra, Rietveld, & Verhoef, 1999; Steg & Vlek, 1997). For example, in a European study, over 90% of the car users supported improved public transport and park-and-ride schemes, while less than 20% approved of reduced parking space and cordon /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 43. VI_2020_008

  .............................................................................................................. 20 3.1 Block Maxima ....................................................................................................................... 21 3.2 Peak-over-Threshold ............................................................................................................. 22 3.3 Estimation /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 44. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 45. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 46. Moellenkampetal_etal-2010

  supported by the majority of responses to one of the quantitative questions (to which 13 out of 20 participants responded on a five-point Likert scale—strongly agree, agree, neither agree or disagree, disagree, strongly disagree), where 11 respondents “agreed” that the activities in the workshop helped them to share their views and opinions with others, and the other two “neither agreed nor disagreed /media/loftslag/Moellenkampetal_etal-2010.pdf

• 47. vanRoosmalen_etal-2009-WRR_2007WR006760

  /a in dry summers, which is the maximum amount licensed by the local government. 80% of the water is abstracted from aquifers located above
  20 masl [Henriksen and Sonnenborg, 2003]. 3. Methods 3.1. Climate-Forcing Data [16] The confidence in Atmosphere-Ocean general circu- lation models (GCM) providing credible quantitative esti- mates of future climate change has increased the past few years /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 48. 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

• 49. IPPC-2007-ar4_syr

  of significant changes consistent with warming Percentage of significant changes consistent with warming 89%94%100% 100% 100% 100% 100% 100% 99%100%98% 96% 91% 94% 94% 90%90%92%94% 355 455 53 119 NAM LA EUR AFR AS ANZ PR* TER MFW** GLO 5 2 106 8 6 1 85 7650 120 24 7645 28,115 28,586 28,671 Changes in physical and biological systems and surface temperature 1970-2004 33 Topic 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf