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77 results were found for k 실시간DB판매Ч〈Tel레Sein07) 실시간디비판매합니다 실시간디비판매 실시간DB판매사이트Д실시간디비판매Ψ실시간DB판매합니다.


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  • 11. Kok_2-scenarios-lecture-2

    Discussion on weighing factors might hamper the creative process. • Being concrete requires expert opinions. Especially when developing a FCM from scratch requires a high level of understanding of all participants. Further reading Kok, K. 2009. The potential of Fuzzy Cognitive Maps for semi-quantitative scenario development, with an example from Brazil. Global Environmental Change 19: 122-133 Van /media/loftslag/Kok_2-scenarios-lecture-2.pdf
  • 12. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 13. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 14. Keranen_Jaana_CES_2010

    tunnisteväriSeuraukset Scenario probability high ACT MONITOR Consequence probabi lity low after control methods PREPARE PREPARE Scenario probability low Consequence probabili ty high after control methods Likely Very unl ikely Very likely Virtuall y certain Unlikely V e r y l i k e l y L i k e l y V e r y u n l i k e l y Excepti onally unlikely = major consequences = moder ate consequences = minor /media/ces/Keranen_Jaana_CES_2010.pdf
  • 15. 2010_005_

    downscaling results previously obtained by Kaas (1993, 1994), as well as results from four different climate models (with the GFDL CM3 as the primary reference). The study found a warming of 0.3 K per decade until the middle of the 21st Century, with a wintertime warming rate of 0.35 K per decade, and a warming rate of 0.25 K per decade in summer. The study also examined precipitation changes and found /media/ces/2010_005_.pdf
  • 16. VI2010-006_web

  • 17. ces-glacier-scaling-memo2009-01

    A reduction in the glaciated area at the lowest altitudes is specified as DSa1 = kDSa ; (10) where k is an adjustable parameter, 0 < k < 1. This reduction is carried out by eliminating the ice-cover sequentially, starting with the lowest elevation band or grid cell of the group and continuing upward until the total eliminated ice-covered area is equal to DS1. Some ice may remain in the uppermost /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 18. Measurements and simulation of volcanic ash for civil aviation

    of Iceland. After registration at 09:00, an opening address will be given by Pétur K. Maack, Director General of Icelandic CAA, at 09:30. Lectures and disscussions will take place until summary at 16:30. The full programme is available as pdf (55 Kb) but the various topics come under these main headings: Ash measurements, experience 2010 and 2011 Initial and boundary data acquisition /about-imo/news/nr/2421
  • 19. isskyrsla_14122010

    15.0W 9) 67 05.0N 21 52.0W 10) 66 57.0N 22 32.0W 11) 67 00.0N 23 00.0W 12) 66 38.0N 25 00.0W 13) 66 30.0N 26 40.0W Næst landi var ísinn á eftirfarandi stöðum: 1. 48 sjml vnv af Grímsey. 2. 46 sjml ana af Horni. 3. 34 sjml norður af Skagatá. 4. 25 sjml nnv af Sraumnesi. Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að sigla í gegnum /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
  • 20. program17012012

    K. Maack, Director General Icelandic CAA Ash measurements, experience 2010 and 2011 9:45 Eruptions in Eyjafjallajökull, Etna and Grímsvötn, airborne OPC measurements and quality assurance Konradin Weber, UAS, Düsseldorf Germany 10:15 Observations in plumes and vicinity of airports Jonas Eliasson HÍ (UI) Initial and boundary data acquisition and improvements in modelling 10:45 /media/vedurstofan/utgafa/hlidarefni/program17012012.pdf

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