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83 results were found for f 계룡타이ㅻ(dm080.com〕 계룡휴게텔❃계룡주점 계룡업소❆계룡유흥.


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  • 71. Cradden_Lucy_CES_2010

    Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf
  • 72. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    Surface 110, F04001, doi: 10.1029/2005 JF000289. Adalgeirsdo´ttir G., Jo´hannesson T., Bjo¨rnsson H., Pa´lsson F. & Sigurdsson O. 2006. Response of Hofsjo¨kull and southern S. Gudmundsson et al. Mass balance of three ice caps in southern Iceland Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 9 (page number not for citation purpose) Vatnajo¨kull, Iceland, to climate change /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 73. Sigurður Th. Rögnvaldsson

    Þorkelsson og Margrét Ásgeirsdóttir 1998. Skjálftahrina í Ölfusi í nóvember 1998. Greinargerð Veðurstofu Íslands VÍ-G98046-JA09. Veðurstofa Íslands, Reykjavík. Sigurður Th. Rögnvaldsson, Kristín S. Vogfjörð og R. Slunga 1999. Kortlagning brotflata á Hengilssvæði með smáskjálftum. Rit Veðurstofu Íslands VÍ-R99002-JA01. Angelier, J., Sigurður Th. Rögnvaldsson, F. Bergerat, Ágúst Guðmundsson, Steinunn S /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/
  • 74. Sigurður Th. Rögnvaldsson

    Þorkelsson og Margrét Ásgeirsdóttir 1998. Skjálftahrina í Ölfusi í nóvember 1998. Greinargerð Veðurstofu Íslands VÍ-G98046-JA09. Veðurstofa Íslands, Reykjavík. Sigurður Th. Rögnvaldsson, Kristín S. Vogfjörð og R. Slunga 1999. Kortlagning brotflata á Hengilssvæði með smáskjálftum. Rit Veðurstofu Íslands VÍ-R99002-JA01. Angelier, J., Sigurður Th. Rögnvaldsson, F. Bergerat, Ágúst Guðmundsson, Steinunn S /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
  • 75. 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
  • 76. VI2010-006_web

  • 77. Kok_JGEC658_2009

    Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.pdf
  • 78. VI_2020_005

  • 79. VI_Arsskyrsla_2018_vef

    Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson. V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8 3 Viðburðaríkt ár er að baki hjá starfsfólki Veðurstofunnar enda felast jafnan margar og fjöl breyttar áskoranir í vöktun og rannsóknum á náttúru - öflum landsins. Loftslagsmál eru mjög á döfinni enda stærsta /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
  • 80. VI_2016_006_rs

    Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

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