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


  • 81. isskyrsla_14122010

    segir hann að þetta er dreifar og þéttur ís hjá honum, lofthiti -5°c. Staður á LLDM er N67.12,10, W020.04,44. LLDM er á leið til Ísafjarðar til að landa rækju þar. Eftir lendingu í Reykjavík upplýsti TFB að LLDM hefði haft samband vegna hafíss. Hafði kl.0030 siglt framá 30-30 metra háan borgarís á stað: 67°10,45´n-020°14,7´v. Sást allvel í ratsjá. Þéttleiki hafíss í næsta nágrenni um 3/10 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
  • 82. norsem_lund

    and Finland. The event was located approximately 59 km SE of Piteå and 80 km NE of Skellefteå in Sweden, while the distance to the nearest Finnish city, Raahe, was 100 km. The earthquake was widely felt in northern Sweden and Finland, the furthest reports come from some 250 km away, with intensities up to V. The main event was followed by 6 aftershocks within the first 8 hours, and two /media/norsem/norsem_lund.pdf
  • 83. VI_2015_005

    Franz Josef Land. The western boundary at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate. Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen to completely include the Barents Sea. This results in an area of 21,625,566 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 84. VI_2020_004

    -CALPUFF model is not using plume height estimates as an input parameter. The model itself solves the equations describing the rising of the mixture in the atmosphere and calculates the top-plume height by using some physical parameters as the vertical mixture velocity (V) and the radius of the vent (R). Based on these two parameters, V and R, we get an estimate of the mass flow rate and we /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 85. Adalgeirsdottir-etal-tc-5-961-2011

    ). Locations of the weather sta- tions, used to reconstruct the temperature and precipitation records, are shown with letters: Reykjavík (R), Fagurhólmýri (F), Hæll (H), Stykkishólmur (S), Teigarhorn (T), Vestamannaeyjar (V), Akureyri (A) and Hólar in Hornafjörður (HH). (B) The surface topography of Vatnajökull ice cap. Dots show the sites of mass balance and veloc- ity measurements, blue dots show /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
  • 86. Daniell_etal-2010

    Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf
  • 87. vanRoosmalen_etal-2009-WRR_2007WR006760

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

    power delivery Finances and risk Financial resources concentrated in structural protection (sunk costs) Financial resources diversified using a broad set of private and public financial instruments Climate change adaptation in European river basins 267 123 Tabl e 2 Overvie w o fvariable s an d indicator s fo rAIW M Dimensio n Variabl e Indicato r Literatur e (A )Agenc y 1. Typ e o fleadershi p /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
  • 89. Hare-2011-ParticipatoryModelling

    O P N O P H ET Sh o w - an d- te ll ve rif ic at io n HE T Us e by deman d OT :Researcher s M M (mode l alread yd ened )M (pa ra m er iza tio n for scenarios ) F M Wadde n Se a Conceptua lmodel s an d simulatio n mode l(DSS ) Im pr o ve m o de l (quality , acceptance , integration ) Po lic y-m ak er s N O P IN D Interview s (conceptua l models ) NO P NO P IN D Dire ct us e (of res u ltin g DSS /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

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