82 results were found for k 관악한잔해ㅍ「zzan1.com〉✏관악퍼블릭✮관악노래방▼관악가요주점 관악2부집✸관악텐.

Results:

• 21. 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

• 22. 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

• 23. 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/

• 24. 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

• 25. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 26. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 27. VI2010-006_web

  /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 28. 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

• 29. 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

• 30. 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