9 results were found for 테고사이언스▷WWW༝S77༝KR▷匼테고사이언스공매도테고사이언스레버리지蓯테고사이언스매도ω🏊🏾‍♀️unreserved/.

Results:

• 1. Protective measures

  experiments for evaluating the effectiveness of avalanche defence structures in Iceland. Main results and future programme (pdf 0,8 Mb) (Í: Proceedings of the International Seminar on Snow and Avalanches Test Sites, Grenoble, France, 22−23 November 2002, F. Naaim-Bouvet, ed., s. 99−109, Grenoble, Cemagref, 2003, author T. Jóhannesson) [abstract] (html) Stálgrindur eða snjóflóðanet? Val á tegund /avalanches/imo/protective/

• 2. VI_2009_012

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 3. Perrels-CBA

  / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf

• 4. VED_AnnualReport-2013_screen

  (). The circulation of Icelandic waters-a modelling study. Ocean Science , –. Nygaard, B. E. K., Hálfdán Ágústsson & K. Somfalvi-Toth (). Modeling wet snow ac- cretion on power lines: improvements to previ- ous methods using  years of observations. Journal of Applied Meteorology and Climatology (), –. Philippe Crochet (). Sensitivity of Icelandic river basins to recent /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 5. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 6. VI_arsskyrsla2020

  fer af stað Í kjölfar fyrstu skýrslu IPCC (Intergovernmental Panel on Climate Change) um loftslagsbreytingar árið 1990 var að frumkvæði vatnafræðisamstarfs innan Norðurlandanna farið af stað með verkefni sem sneri að áhrifum loftslags- breytinga á vatnafar og vatnsorku. Verkefnið hófst 1991 og var ármagnað af Norrænu ráðherranefndinni. Niður- stöður þess voru skýrar: Ef fram færi sem horfði /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 7. vonKorff_etal-2010

  the step when this appeared necessary for comparability, and explained the substep according to the descriptions by the authors of the guide. In the fourth column of the author tables, we noted which substeps in the other guides corresponded to the substep under examination, which brings us to reconstruction. In three “reconstruction tables” (Appendix 2: Tables A2-1–A2-3), we recombined the results /media/loftslag/vonKorff_etal-2010.pdf

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

  on the European level [e.g. Water Framework Directive (Directive 2000/60/EC), Common Agricultural Policy, etcetera], except for the Ukrainian part of the Tisza. However, the Ukraine shows strong incentives to enter the EU community and thus the EU acquis communautaire is used as key reference for the development of its water management principles. It was nevertheless decided to select two case-studies /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 9. 2010_003rs

  A (A1, A2, A3). ........................................................................................... 89 Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90 Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90 Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf